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Acid-Base Disturbance Cases

ZACHARY R. HEALY

• Includes 75 real-life progressive cases to facilitate knowledge application

• Includes interpretation of triple-base disturbances

• Answers include rich rationales that explain both correct and incorrect answers

• Targets a vast array of topics in internal medicine and critical care

CRITICAL CONCEPT MASTERY SERIES

Acid-Base Disturbance Cases

NOTICE

Medicine is an ever-changing science. As new research and clinical experience broaden our knowledge, changes in treatment and drug therapy are required. The authors and the publisher of this work have checked with sources believed to be reliable in their efforts to provide information that is complete and generally in accord with the standards accepted at the time of publication. However, in view of the possibility of human error or changes in medical sciences, neither the authors nor the publisher nor any other party who has been involved in the preparation or publication of this work warrants that the information contained herein is in every respect accurate or complete, and they disclaim all responsibility for any errors or omissions or for the results obtained from use of the information contained in this work. Readers are encouraged to confirm the information contained herein with other sources. For example and in particular, readers are advised to check the product information sheet included in the package of each drug they plan to administer to be certain that the information contained in this work is accurate and that changes have not been made in the recommended dose or in the contraindications for administration. This recommendation is of particular importance in connection with new or infrequently used drugs.

CRITICAL CONCEPT MASTERY SERIES

Acid-Base Disturbance Cases

Zachary Healy, MD, PhD

Assistant Professor

Division of Pulmonary and Critical Care Medicine

Department ofMedicine

Duke University Hospital

Durham, North Carolina

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This collection of clinical acid-base cases is meant to sharpen clinical skills in evaluating such disorders. We aim to do so by providing a structure for the evaluation of acute and chronic, primary and secondary acid-base disturbances, as well as approaches to identify the underlying etiologies. This series was conceived to provide cases with a level of complexity that would appeal not only to medical students, but also to residents and fellows, and it will intermittently include questions regarding the most appropriate treatment of patients after identifying the aforementioned acidbase disturbances. Although basic physiologic explanations are provided throughout, this text is not intended to replace essential physiology texts. References to such texts and supplemental peer-reviewed literature are provided throughout where appropriate. Following are a few notes prior to diving into the approach.

While the approach to analysis provided herein may appear rather black-and-white, real-world acid-base interpretation is often less clear, with plenty of gray area. This may be due to a number of issues, including the timing of laboratory studies, the growing use of point-of-care testing and venous blood gas data in the initial evaluation of patients, and limitations of the linear equations describing respiratory and metabolic compensation, among others. Importantly, we typically lack the necessary quantitative information to define the chronicity of acid-base disorders, which then makes interpretation of the acute disorders much more difficult. In such cases, we are required to make assumptions that potentially introduce additional error. For instance, in the first case in this series, you will see how a priori knowledge of a chronic respiratory acidosis can significantly alter the interpretation of metabolic acid-base disturbances (and underlying etiologies) in critically ill patients.

All of the cases presented here have been interpreted using the "bicarbonate" (or "Boston") approach introduced by Relman and Schwartz, as opposed to utilizing the base excess (BE) approach introduced by Siggard-Anderson, the standard base excess (SBE) introduced by Van Slyk.e, or the more complex Stewart approach to acidbase physiology. Each of these approaches will be briefly discussed. While there has much debate regarding which of the bicarbonate and Stewart approaches to acidbase physiology provides the greatest diagnostic and prognostic information, studies comparing the two methods have been largely inconsistent or shown clinical equivalence. As the bicarbonate approach remains the most popular approach taught in medical education and does not require simultaneously solving multiple equations, this approach will be utilized throughout the text. Additionally, we realize that there are multiple variations and short-hand versions of the equations used to determine the "delta-delta" as well as appropriate metabolic and respiratory compensation. While many of these variations or shorthand rules will produce the same or similar

mathematical result, the physiologic principles underlying them are often lost or at least less transparent. 1bis can often lead to transposition of terms or general confusion in less-experienced clinicians, and such shorthand should be reserved for more experienced practitioners. This text will utilize a consistent equation-based approach for all calculations, and all necessary equations will be provided in the introduction (as well as in the solutions to the case problems}.

Next, one of the most important aspects of acid-base interpretation is the application of common sense, particularly with regard to taking the patient's medical and social history into account. This cannot be overstated. For instance, an otherwise-healthy, elderly patient presenting with an infiltrate on chest film, fever, productive cough, hypotension, and an elevated anion gap acidosis is most likely to have a lactic acidosis secondary to sepsis rather than toluene toxicity from inhalation drug abuse. And while it is always important to keep an open mind when formulating a differential diagnosis, common diagnoses will remain common; you will encounter lactic acidosis and diabetic ketoacidosis (DKA) much more frequently than cyanide or carbonmonoxide poisoning in practice. Finally, recall that most of the acid-base disorders encountered throughout medicine (and this text) are in critically ill patients; it is therefore not always possible to await confirmatory testing before instituting treatment decisions, and such decisions about diagnosis and treatment will often be based on imperfect information.

PROCESS OF EVALUATION

The first step in the evaluation of the acid-base status is the clinical evaluation. This should include a detailed history of the present illness, with particular attention to the timing/duration of the patienfs symptom onset. In patients who are incapacitated or encephalopathic, this should also include a detailed history of the environment in which the patient was found (eg, prescription medications, over-the-counter [OTC] medications, bottles of industrial cleaner, running vehicle, etc) as well as any collateral history that is available. Additionally, it is important to include a detailed review of systems with particular attention to those symptoms that could contribute directly to an acid-base disorder (eg, emesis, diarrhea, pain, etc). A prior medical and surgical history is also critical, with particular attention to conditions associated with chronic acid-base disorders (eg, chronic renal insufficiency, chronic obstructive pulmonary disease [COPD], history of abdominal or pelvic surgery), and a history of prior suicidal ideation or suicide attempts. A complete medication list must also be obtained, including OTC medications and herbal or dietary supplements. An appropriate social and environmental history should include any history of substance abuse (alcohol, opioids, benzodiazepines, etc) and hobbies. A complete physical examination should also be included in the evaluation.

The next step in the evaluation process is to ensure that the appropriate or necessary data are available. This should include an arterial blood gas (ABG) analysis (including pH, Paco2, and Pao2 ), as well as a serum basic chemistry panel (sodium [Na], potassium [K], chloride [Cl], carbon dioxide [C02 ], blood urea nitrogen [BUN], creatinine [Cr]), and a serum albumin. These should be drawn at the same time or in very close proximity, and if possible prior to intervention. While a peripheral venous blood gas (VBG) or central venous blood gas analysis may also be used for evaluation of acid-base status, note that this can introduce error into your calculation. Table 1-1 provides some general guidelines for correlating ABG and VBG values.

If the laboratory data do not match the clinical situation, check for potential laboratory errors in terms of the patient identification. Also, be alert to the potential for venous blood samples to be contaminated or diluted with intravenous fluids, particularly if a solution or medication is infusing distal to the site of venipuncture. The ABG can often be helpful here as arterial samples should not be affected by infusions and should therefore represent the clinical situation. Importantly, note that the reported bicarbonate (HC03 ) in an arterial or venous blood gas is a calculated rather than a measured value. Also note that the C02 from the serum chemistry panel represents the total C02 in the serum sample; since the majority(> 95%) ofC02 is transported

TABLE 1-1

• Differences between arterial, peripheral venous, and central venous blood gas values.

Relative to ABG pH

Pco2 mm Hg [HCO;l (mEq/L)

Peripheral VBG [0.03--0.04] lower [2-1 o mm Hg] higher [1-2 mEq/L] lower than thanABG thanABG ABG

Mixed or [0.02--0.06] lower [3-6 mm Hg] hlghar [-1 to 1 m Eq/U centralVBG thanABG thanABG different (no difference)

ABG, amrlal blood gas; HCO;, bkarbonate; Pco,. partial pressure ofcarbon dioxide; VBG, venous blood gas.

in the form ofHC03, we generally use the value reported for the C01 as the serum HC0 3• In the case of suspected pseudohyponatremia, remember to use the measured value rather than the corrected value in your studies. Finally, note that some substances can interfere with test results. Namely, hypertriglyceridemia or cell lysis can significantly alter lab values. Similarly, some metabolites of ethylene glycol and methanol can interfere with lactate determination, depending on the lab. Also, to check for internal consistency, one can use the Henderson-Hasselbach equation to ensure that the pH, partial pressure of carbon dioxide in arterial blood (Paco2 ), and HC0 3 values are consistent: [ ] HCO, [ l [[HCOJ]

pH= 6.1 + log10 ; or pH= 7.61 + log10

0.0307 * Paco 2 Paco 2

While the normal value for arterial pH can range from 7.35 to 7.45, patients with appropriate compensation can havevalues within this range, and therefore acid-base disorderscan oftenbemissed. Consequently, for the purpose ofthe text, we willconsider the normal range to be 7.38 to 7.42. Similarly, the normal values for HC03 range from 21 to 27 mEq/L, with a median value of24 mEq/L; in order to prevent missing a potentialacid-base disorder, wewilluse a normalrange of22to 26 mEq/L. The normal range for Paco2 is between 35 and 45 mm Hg with a median value of 40 mEq/L, although we will use a normal range of38to 42 mm Hg.

Thenextstep in the evaluation processis an attempttoidentifythe patient's"baseline" acid-base statusbydefiningany existingchronic acid-base disorders,ifpossible. This generally requires evaluation of a patient's prior laboratory data and/or an available blood gas when the patient was at baseline health. Tiris is particularly important for patientswith chronicrespiratoryacidosis, as,in additiontoanelevatedbaselinePaco2, the patient's"baseline"HC03 (andhence the chloride) canbesignificantlyaltered from that of"healthy" or "normal" patients. For example, assume you have a patient with advanced COPD who presents to the emergencydepartment with blood gas values of pH 7.25, Paco2 65 mm Hg, and HC03 27 mEq/L. The interpretation ofthis patient's blood gas, if we assume the patient has a "normal" baseline (eg, Paco1 40 mm Hg, HC03 24 mEq/L) would be an acute respiratory acidosis with an appropriate renal

compensation; however, if you know that the patient has a chronic respiratory acidosis with a baseline acid-base status of pH 7.30, Paco2 65 mm Hg, and HC0 3 36 mEq/L, you would be able to accurately diagnose that the patient has an acute metabolic acidosis, with an acute-on-chronic respiratory acidosis. In the first case, we were forced to assume a normal baseline, and this would have caused us to miss that patient's metabolic acidosis initially, which could potentially be catastrophic. This is particularly important in chronic respiratory acid-base disorders, where both the Paco and the HC03 are altered. While some references suggest that the ratio [HCO)]/tPaco2 ] can be used to determine if a respiratory process is acute or chronic, this ratio does not provide a 1:1 mapping to a particular set of acid-base disorders. For example, consider a patient presenting with a respiratory acidosis that has a ratio of 0.2. Based on Figure I-1, this patient may have an acute-on-chronic respiratory acidosis with or without a metabolic acidosis/alkalosis, an acute respiratory acidosis with a concomitant metabolic alkalosis, or a chronic respiratory acidosis with an acute metabolic alkalosis.

Unlike compensation in chronic respiratory acid-base disorders, the compensation in chronic metabolic acid-base disorders is poorly characterized and inefficient; therefore, it is less important to identify these conditions initially.

The next step is to determine if the primary issue is an acidemia or alkalemia. This is another instance where common sense must be utilized. While the normal value for the arterial pH may be between 7.35 and 7.45, multiple acid-base disturbances may still be present in a patient with a pH in this range. Therefore, it is important that one does not

AcutB n111plrmay acldoals with appropriate metabolic compensation

AculB r1111plratory acidosis with metabolic alkalosis : AculB rellpiratory acidosis with rnatabollc acldoals 1---------------1--- Acute-on-dlronlc n111plrmory acidosis with metabolic alkalosls +--- 0.'1 --=-

Acuta-on-dlronlc 1'88plratory acldoals (with approprtata compensation for each phase)

Aoot&-on-chronic l'llSpiratory 4.--+---------------1 and no metabolic component acidosis with metabolic acidosis --+ Chronic r1111piratory acidoaia with metabolic alkalosia

Chronic rasplratory acidosis 4,--+---------------1 with metabolic acidosis

Chronic n111plrmory acldoals with approprtllls rnatabollc compensation

Figure 1-1 • Potential combinations of acute and/or chronic metabolic and respiratory disorders that may be seen at different ratios of the change in serum bicarbonate (HC03) to the change in arterial co2.

Metabolic Acidosis

Go to metabolic acidosis flowchart

Healthy Palietlt:

Baseline Acid-Base Disorder?

Define new baseline 1111W'or HC03 ••Parficularly helpful lo identify chronio rNpifatary 11Cid03is

Ensure Quallty/Tlmlng ot Data

ABG and serum veno chemistry drawn at similar time

oontinuewith

Respiratory Acidosis Go 1o respiratory acidosis flowchart

Respiratory Alkalosis Go to respiratory alkalosis flowchart

Baseline 21-28 mEq/L, although we Bll8ume a median value of 24 mEq/L Ballellne Pac:o2: 30-45 mm Hg, atthough we assume a median value of 40 mEqlL

Chronic Acid-Base DisotrJ9r:

Replace the values in red in the flow chart with the patient's baseline values

Figure 1-2 • Initial algorithm for the evaluation of acid-base disorders.

Metabolic Alkalosis

Go 1o metabolic alkalosis flowchart

examine the pH, see that it is 7.39, and assume that no acid-base disorder is present. For example, a patient recently presented to our emergency department with a pH of 7.39, Paco2 of25 mm Hg, and serum HC03 of15 mEq/L and the diagnosis ofan acute pulmonary embolus with cor pulmonale. Although the patient's pH was normal, this was due to the presence of an anion gap acidosis due to lactic acidosis secondary to cardiogenic shock and a concomitant respiratory alkalosis. Therefore, it is important to analyze the pH, Paco2, and serum HC03 for every patient. Although we examine the pH first, this is simply to provide some guidance as to what the primary acid-base disorders are in any given patient If the pH is in the range of 7.39 to 7.41, it may not be possible to determine which is the primary process. The next step is to determine the primary processes present, followed by examination for appropriate compensation and identification of any secondary acid-base disorders present. Recall that even with "'complete" compensation, the arterial pH does not reach 7.40; this is a common misconception, and therefore we will use the term "appropriate" rather than "complete" compensation throughout the text. Respiratory compensation is driven by pH changes in the cerebrospinal fluid, leading to alterations in the respiratory centers. Metabolic compensation is driven by pH-sensitive cells in the renal tubules. Once one has identified all existing primary and secondary acid-base disorders present, one must go through each decision tree to attempt to identify the etiologies responsible for each disorder, as this will guide treatment decision making (see Figure 1-2) Again, it is also important to identify patterns of disorders that are associated with particularly etiologies. For example, aspirin toxicity can be associated with a respiratory alkalosis and an anion gap acidosis.

METABOLIC ACIDOSIS

Figure1-3 represents the algorithm for apatientwitha metabolic acidosis.

Metabolic Acidosis i

Is the respiratory compensation appropriate?

Eitpectsd Paco2 = 1.5 • [actual HCOs] + 8 ± 2 (In mm Hg)

Concomitant AellplralDry Acldalllll Approprlllle Compenallllon CoMomllllnt ReaplralDry Alkaloals rwplmory acidosis flow chart rupRml)' .a.tosis flow chart

Cornicllon at axpac:llld anion a•P tar •rum albumin

Expected Anion Gap = 12 - (2.5) • [4.0 :L -Actual Serum Albumin]

iSwum Anion Gap (SAG)

SS1Um Anion Gap (SAG) = [Na+] - [HC03] - [Gr]

Anion Gap =Sfl/1Jm Anion Gap - Eitpectsd Anion Gap

Non-Anion G•p Acidosis (NAGMA) AChOmEqll.

Significant Anion Bap Acldm/a p,_f?

Urine pH < 11.5?

·-(MAllllA) -

Urine [Na]+ < 20 mEq/l (pool" ,.,.., dlat.I Na drlllvwy) v i allhll-

Urln• Oamolal Gmp (UOG) Calc:ulallon ......

Figure 1-3 • Algorithm for evaluation of a metabolic acidosis.

NolDoll ollhll-

Urlne Anion Gmp (UAG) Calculation ........

The first step in a patient with a metabolic acidosis is to determine if the compensation is appropriate. For a metabolic acidosis, we do not differentiate between acute and chronic when determining the compensation, as the respiratory compensation for a chronic metabolic acidosis is poorly defined and generally inefficient. The equation we will use, called the Winter equation, is generally accurate for a serum HC03 between 5 and 22 mEq/L:

Expected Paco2 "' 1.5 * [Actual HC03] + 8 ± 2 (in mm Hg).

Respiratory compensation for a metabolic acidosis begins within minutes and is "complete" within 12 to 24 hours. If the Paco1 falls within this range, this is termed an "appropriate" or complete respiratory compensation, and no respiratory acid-base disorder is present. If the Paco 2 is lower than the expected range, there is a concomitant respiratory alkalosis, whereas if the Paco1 is higher than the expected range, a concomitant respiratory acidosis is present. The limit of respiratory compensation is between 8 and 10 mm Hg. Once this has been determined, the next step is to determine if an anion gap acidosis is present. The first step in determining if an anion gap is present is to calculate the expected or "normal" anion gap. The serum anion gap

represents the unmeasured anions in the serum. In the most basic form the serum anion gap is calculated as follows:

Serum Anion Gap= [Na+) - - [Cl-],

In which the units of measure are milliequivalents per liter (mEq/L). Recall that the milliequivalent (mEq) is a measure of net charge (or valence), so 1 mmol of potassium is equal to 1 mEq, whereas 1 mmol of calcium, which carries a net charge of 2+, is equal to 2 mEq. Therefore, in this form, the unmeasured anions include albumin, phosphorus, lactate, bromide, and negatively charged monoclonal proteins. Phosphorus exists as an anion in the form of monohydrogen and dihydrogen phosphate (HPO!- and Hl0;:). There are also unmeasured cations, which include potassium, calcium, magnesium, and positively charged monoclonal proteins. Since magnesium, phosphorus, calcium, and potassium are often measured, one could write the equation as:

SerumAnionGap= [Na+]+ [K+) + [Ca2+) + + [cl-J-[P"-1] (in );

Alternatively, if the values are in mrnol,

If the values are in milligrams per liter (mg/L), this can be converted using the molecular weights (mg/mrnol or g/mol): for calcium, 40.1; and for phosphorus, 31. Recall that both phosphorus and calcium are typically expressed as mg!dL, so to convert from mg/dL to millimoles per liter (mmol/L), multiply the calcium value by 0.401 and the phosphorus by 0.31 to covert to mmol/L In an otherwise healthy patient, these other unmeasured cations and anions generally cancel out; therefore, the major anion responsible for the anion gap is albumin. For the most common form of the serum anion gap equation (including only sodium, serum HC0 3, and chloride), we must correct the expected anion gap for the patient's serum albumin, using the following equation:

Expected Anion Gap = 12 - (2.5) * [ 4.0 ! -Actual Serum Albumin J.

While the expected anion gap is -12 mEq/L for an otherwise healthy patient with a serum albumin of 4.0 gldL, this value will be lower in patients with hypoalbuminemia. There are conditions that can be associated with a low anion gap ( < 3 mEq/L), as well as those associated with a negative anion gap. Some of these conditions are provided in Table I-2.

After determining the expected anion gap and calculating the serum anion gap, one can determine the anion gap (AG):

Anion Gap = Serum Anion Gap (measured) - Expected Anion Gap (in .

TABLE 1-2

• Unmeasured cations and anions, conditions associated with a low or negative serum anion gap, and other potential anions that may be present in a patient with one of these conditions.

Common Unmeasured Cations

• [K•]

• [Ca>+]

• [Mg>+]

• Monoclonal protein accumulation (some lgG forms)

Common Unmeasured Anions

• Phosphorus

• Lactate

• Bromide/iodide

•Albumin

• Monoclonal protein (lgM)

Causes of a Low Serum Anion Gap 3 mEq/L)

• Laboratory error

• Hypoalbuminemia

• Severe NAGMA

• Lithium toxicity

• Monoclonal gammopathy, multiple myeloma

• Bromide/Iodine Ingestion (Interferes with serum [Cl-] measurement)

• Pseudohyponatremia

• HCO, infusion (chloride-deplete solution)

Causes of a Negative Serum Anion Gap

• Hyperlipidemia (falsely elevates serum [Cl-] measurement)

• Bromide Ingestion

• Pyridostigmine use

• Salicylate intoxication

NAGMA, non-<in/on gap metabolic acidosis.

If the anion gap is positive, this indicates that an anion gap acidosis is present, whereas if the value is zero or less than zero, there is no anion gap acidosis, and only a non-anion gap acidosis is present. At this point, it may be prudent to order some additional laboratory studies pending the patient's presentation and other clinical history (see Table 1-3) .

TABLE 1-3

• Additional laboratory studies to consider for an anion gap and non-anion gap acidosis.

Anion Gap Acidosis

• Complete blood count with dlfferentlal

• Serum lactate (either arterial or venous)

• Urine drug screen

• Serum drug screen, which should include

Non-Anion Gap Acidosis

• Urine electrolytes (Na, K, Cl)

• Urlnalysls

• Urine osmolality

• Urine urea ethanol, salicylates, and acetaminophen levels

• Liver function testing

• Serum osmolality

• Serum acetone or ketones (beta-hydroxybutyrate)

DELTA-DELTA CALCULATION

For a patient with an anion gap acidosis, the next step is to determine ifthe patient has a pure anion gap acidosis, or there is also a concomitant non-anion gap acidosis or a metabolic alkalosis. This is determinedbyusingthe delta-delta (.6..6.):

M = (CalculatedAnion Gap)- (Expected Anion Gap).

(Expected Serum C02)-(Actual Serum C02)

The delta-delta equation compares the size ofthe anion gap to the magnitude of change in the serum HC03 • Recall that one should use the serum HC03 as a surrogate for the serum C02 • Additionally, for the expected serum HC03, one should use the patient's baselineserum HC03 ifitis known to be different than 24 mEq/L. For patientswith a pureaniongap, the ratio is generallybetween 1.0and2.0. Recall that a strong acid dissolves in blood to an anion and a hydrogen molecule. The hydrogen molecule reacts with an HC03 molecule to yield a water molecule and a molecule ofcarbon dioxide. Therefore, for each molecule ofacid, the change in anion gap would be balanced bythe loss ofan HC03 molecule, yielding a 1:1 ratio. However, this requires that renal function is maintained, and that the excretion of anion and the acid component of strong acid are equal overall. Additionally, the hydrogen ion released from the strong acid can also be buffered by bone or within cells, and therefore the anion gap will be higher than the reduction in the serum HC03 • Obviously, as the serum HC03 level is further reduced, more of the acid will be buffered by other means. Therefore, the delta-delta ratio can be elevated up to a value of2.0 and still represent a pure anion gap acidosis. A value of 1.6 is commonlyseeninpatients with apure typeA lacticacidosis. It is important to note here thatthe body does not producelactic acid; rather, hydrogen ions are produced aspartofthe anaerobic metabolism pathways thatlead to lactate anion production. Therefore, the ratio here is not 1:1. Additionally, many ofthe conditions leading to a lactic acidosis (type Alacticacidosis) are also associated withreduced renal function (leadingto animbalance in anion and acidexcretion) and more severeacidosis (which pushes more H+ to be buffered in the bone and intracellularly).

Patients with a value less than 0.4, despite having an elevated anion gap are more likely to have a pure non-anion gap acidosis without an actual anion gap acidosis. This is simplydue to the limitsofthe equations we use to describe much more complex physiology. In this case, the reduction in the serum HCO3 significantly outweighs the increase in the anion gap. This scenario is usually seen in patients with a very small butpositiveanion gap, buta significantreductionin serumHC03, suchas a type 1renal tubular acidosis (RTA).

Patients with a value between 0.4 and 0.9 are diagnosed with a mixed anion gap and non-anion gap acidosis. Patients with a value greater than 2.0 are diagnosed with an anion gap acidosis and a metabolic alkalosis. For each additional acid-base disorder present, one must pursue a diagnostic workup based on the provided algorithms. terpretation ofdelta-delta values.

<0.4

0.4-0.9

1.0--2.0

>2.0

SERUM OSMOLAL GAP

Non-anion gap only

Anion gap and non-anion gap acidosis

Anion gap acldosls only

Anion gap acldosls and metabolic alkalosls

Once the delta-delta evaluation is completed, a serum osmolal gap should be calculated. While this is not necessary in patients with a clearly identifiable cause and consistent clinical history, we generally include this as part of the algorithm to prevent this step from being missed, as the timely identification of an anion gap acidosis with a serum osmolal gap is critical to preventing significant morbidity. The serum osmolal gap is important for determining whether toxic alcohol ingestions have occurred. First, we calculate the serum osmolality (equivalent to the expected anion gap calculation). Again, as with the serum anion gap calculations, there are a number of ways this can be written, which can include additional variables. The most significant solutes in plasma are sodium, HC0 3, chloride, glucose, urea, and ethanol. Therefore, the most common form is written as follows:

where the units are as follows: serum osmolality, mOsm/kg (which is equivalent to the serum osmolality when written mOsm/L of water, as 1 L of water weights 1 kg) ; Na, mmol/L; glucose, mg/dL; BUN, mg/dL; ethanol, mg/dL. The conversion factors for glucose, BUN, and ethanol shown in the preceding equation convert the units from mg/dL to mOsm/kg. The sodium value is doubled to use as a surrogate for the chloride and HC0 3 values. The following are additional terms (with conversion factors) that may be used in the equation if the values are measured in milligrams per deciliter (mg/dL) : methanol, 3.2; isopropyl alcohol, 6.0; ethylene glycol, 6.2; acetone, 5.8. Finally, if the beta-hydroxybutyrate or lactate are measured, they may be included directly (without conversion) in units of mmol/L.

Using the more common formulation for the calculated serum osmolality, we can determine the serum osmolal gap by measuring the serum osmolality:

Serum Osmolal Gap = Measured Serum Osmolality - Calculated Serum Osmolality.

The serum osmolal gap, when normal, should fall in the range of -10 to + 10 mOsm/kg. Anything greater than +10 mOsm/kg is considered a positive serum osmolal gap, and a value greater than + 15 mOsm/kg is generally considered a critical value. Table 1-5 includes conditions that can lead to an increased serum osmolal gap with and without a concomitant serum anion gap acidosis.

TABLE 1-5

• Conditions associated with an el11Yated serum osmolal gap with or without an associated anion gap acidosis.

With an Elevated Serum Anion Gap

1. Ethanol ingestion with alcohol ketoacidosis (acetone is an unmeasured osmole, in addition to ethanol)-the osmolallty Is usually elevated more so by the Increased ethanol concentration, so the osmolal •gap" depends on whether the term for ethanol ls included in the osmolallty calculation'

2. Organle alcohol Ingestions (methanol, ethylene glycol, dlethylene glycol, propylene glycol)

3. OKA-similar to ethanol ingestion, earlier, glucose and acetone contribute to the osmolality, since the glucose term is always included in the calculation

4. Salicylate toxicity

5. Renal failure-the BUN Is nearly always included in the osmolallty

Without an Elevated Serum Anion Gap

1. Hyperosmolar therapy (mannitol, glycerol)

2. Other organic solvent Ingestion (eg, acetone)

3. lsopropyl alcohol ingestion (produces only acetone rather than an organic acid, so no anion gap is seen)

4. Hypertriglyceridemia

5. Hyperprotelnemia

'A mildly elevated osmolol gap hos been reported in the literature in patients with lactic acidosis in critical illness, particularly sl!\ll!re distributive shock. The pathology is not quite clear, although it likely is related to multiorgon failure-particularly involving the liver and kidneys-and the release ofcellular components known to contribute to the osmolol gap. This is typically around 10 mOsmll., although it may be as high as 20--25 mOsm!L

ANION GAP ACIDOSIS

Once all the calculations for the anion gap acidosis portion of the algorithm have been performed, one can attempt to determine the underlying etiology. Common and less common causes of an anion gap acidosis are provided in Tables I-6 and I-7.

Lactic acidosis, DKA, and chronic renal insufficiency/failure remain the most common forms of anion gap acidosis seen clinically. Lactate, which is produced from anaerobic metabolism, can then be converted back to glucose in the liver via the Cori cycle, excreted as an anion in kidney, or used in the Kreb cycle via conversion to pyruvate. L-Lactic acidosis can be classified into type A and type B; a separate form of acidosis,

TABLE 1-6 • Causes of anion gap metabollc acidosis.

Common

Lactic acidosis (lncludlng transient)

Renal failure [•uremia")

OKA

Alcohol ketoacidosis

Starvation ketoacldosls

Salicylate poisoning (ASA)

Acetaminophen poisoning (paracetamol)

Organic alcohol poisoning (ethylene glycol, methanol, propylene glycol)

Toluene poisoning ("glue-sniffing")

Less Common

Cyanlde poisoning

Carbon monoxide poisoning

Aminoglycosides

Phenformin use

0-Lactlc acidosis

Paraldehyde

Iron

lsoniazid

Inborn errors of metabolism

TABLE 1-7

• Anions/metabolites associated with different causes of an anion gap acidosis.

Methanol -7 Formic acid

Ethylene glycol -7 Oxalic acid

Propylene glycol' -7 D-Lactic acid (potential metabolite)

Toluene -7 Hippuric acid

Ketoacldosls -7 Ketones (acetoacetone, beta-hydroxybutyrate)

Aspirin -7 Salrcylates

Acetaminophen -7 5-0xoproline (pyroglutamic acid)

Cyanide -7 2-Aminothiazoline-4-carboxylic acid (ATC)

•Pharmacologic Agents Potentially Utilizing Propylene Glycol

• Lorazepam

• Phenobarbital

• Bactrim

• Esmolol

• Nitroglycerin

termed D-lactic acidosis, occurs as a by-product of bacterial metabolism in patients with specific risk factors. Type A lactic acidosis is seen more commonly, and is associated with evidence of poor tissue perfusion or oxygenation, whereas type B lactic acidosis is typically associated with delayed clearance or tissue utilization of lactate. Causes of a type A lactic acidosis includes shock, limb ischemia, carbon monoxide, and severe hypoxemia. Causes of a type B lactic acidosis include liver/renal failure, malignancy, drug toxicity, and inborn errors of metabolism. Type D-lactic acidosis can result from bacterial metabolism in patients with reduced small bowel absorption (short-gut syndrome, gastric bypass with small bowel resection). It usually occurs after a large carbohydrate load but may also be seen in patients with DKA (via metabolism of methylglyoxal) or patients receiving infusions of medications containing propylene glycol. D-Lactate is filtered freely and is not well resorbed in the proximal tubule.

Patients with a ketoacidosis usually have preserved renal function. The anions are excreted as salts with sodium or potassium rather than with ammonium. The administration of glucose (and insulin in DKA) reduces the production of ketone bodies, while the administration of isotonic fluids leads to increased anion and acid excretion (along with sodium, but not chloride). The anion gap is therefore usually "closed" or resolved by a shift to a non -anion gap acidosis.

Chronic kidney disease (CKD) may be associated with a non-anion gap acidosis, a pure anion gap acidosis, or a mixed anion and non-anion gap acidosis. Early in the disease process, acid excretion is more significantly impacted than anion excretion, leading to a non-anion gap acidosis. As the disease progresses, there is more impact on anion excretion, leading to a mixed or pure anion gap acidosis.

NON-ANION GAP ACIDOSIS

The primary etiologies for a non-anion gap acidosis include acid ingestion/infusion, RTA, and gastrointestinal (GI) losses of HC0 3• Aside from the history, the primary tools for determining the etiology of a non-anion gap acidosis are urine studies, including the urine pH, presence of kidney stones, the urine anion or osmolal gap,

and the serum potassium. Approximately 50 mEq of non-volatile acid is excreted by the kidneys on a daily basis, although they are capable ofhandling up to 10-fold increase in acid load. Renal acid excretion occurs predominantly via conjugation ofhydrogen ions to ammonia, forming ammonium (NH;). Therefore, the normal response to ametabolic acidosis is to increase NH; excretion,thus reducing the urine pH (typically< 5.5). This acid excretion primarily occurs in the distal tubules and collecting duel In a type 1 (distal) RTA, type 4 RTA, and CKD, patients will have reduced ammonium excretioninresponse to anacidload.Itis importantto differentiate these conditions from those diagnoses associated with a loss ofHC03 via either the GI tract or the kidney. In a proximal RTA, there is defective resorption ofHC03 in the proximal tubule, which may be accompanied by other abnormalities in the proximaltubule. In diarrhea, HC03 andpotassium are lostviathe GI tract.

Inorderto differentiatebetween GI lossesofHC03 and reducedrenalacid excretion, one may use a surrogate measure ofserum ammonium excretion, in addition to the urinary pH. Although some facilities can directly measure the urinary ammonium, many cannot. Therefore, there are two primary options for estimating the urinary NH; excretion: the urine anion gap and the urine osmolalgap.

The urineanion gapprovides anindirectestimate ofthe urine ammonium excretion. The urine anion gap is calculated as follows:

Urine Anion Gap =Na:ru,_ + K:ru,.- Cl•

The typical value ofthe urine anion gap is between +10 and +100mEq/L in patients consuming a Western diet Urinary chloride is most commonly excreted in complexwith sodium, potassium, or ammonium ions. Therefore, in a patient with intact urinary acidification, as urinary ammonium excretion increases, more chloride is excreted, and the urine anion gap will become more negative. In patients with a GI source ofHC03 loss such as diarrhea, the urine anion gap will be considerably negative, typically between -20 mEq/L and -50 mEq/L. Alternatively, in patients with dysfunctional urinary acidification, the urine ammonium excretion will not increase significantly,and the urine aniongap will remain positive, usuallywithin the normal range (+10 to +100 mEq/L). A valuebetween-20 and +10 is generally inconclusive.

There are several limitations to the use ofthe urine anion gap. First, the urine anion gap can also be impacted by the excretion of other unmeasured anions not usually present in the urine, so it should be used with significant caution in patients with a concomitantanion gap acidosis.Inthese patients, the unmeasured anion (eg, lactate, hippurate, 5-oxoproline, etc) will serve to falsely elevate the urine anion gap. Additionally, the presence ofpolyuria or a urine sodium level less than -10 to 20 mEq/L can also make the urine anion gap less reliable.

An alternative to the urine aniongap is the urine osmolal gap. The urine osmolalgap is calculated in a manner similar to the serum osmolalgap:

The urine osmolal gap should be proportionate to the urinary ammonium, as this is the only other major urinary solute not included in the above-calculated urine osmolality (recall that vast majority of unmeasured anions will be complexed with either sodium or potassium, which are included here). Therefore, the urine osmolal gap is a more direct measure of the urine ammonium excretion. A normal value in a patient with a normal acid-base balance falls between 10 and 100 mOsm/kg, although in patients with an RTA these values are usually on the low end of this spectrum ( < 20 mOsm/kg). When faced with an acid load, a patient with intact urinary acidification (ie, diarrhea) will significantly increase the urine ammonium excretion, and hence the urine osmolal gap will also increase significantly (> 400 mOsm/kg). Since the ammonium must be also be complexed to an anion for excretion, the urine ammonium concentration can be estimated as one-half of the urine osmolal gap (ie, for a urine osmolal gap of 400 mOsm/L, the urine ammonium concentration would be estimated as 200 mOsm/L). Generally, the urine osmolal gap will not exceed -600 mOsm/L. Alternatively, in a patient with dysfunctional urinary acidification (ie, type 1 or type 4 RTA), the serum osmolal gap will not exceed 150 mOsm/kg.

Similar to the urine anion gap, there are limitations to the use of the urine osmolal gap. First, the urine osmolal gap should not be used in a patient with increased urinary excretion of non-ammonium solutes (eg, mannitol methanol), which would yield a potentially inappropriate elevation in the urine osmolal gap. Additionally, a urinary tract infection with a urease-producing bacteria can lead to inappropriate elevation of the urine osmolal gap, as urea can react with water to produce ammonium and HC03 , depending on the urine pH.

Once the urine anion gap or urine osmolal gap have been determined, the urine pH, serum potassium, presence of renal stones, and other abnormalities of the urinalysis can be used to determine the most likely diagnosis and underlying etiology. However, it should also be noted that the urine pH is not helpful in differentiating the etiology in chronic or prolonged metabolic acidosis that is also associated with hypokalemia (eg, chronic diarrhea). in severe volume depletion, or in patients with urinary tract infections secondary to urease-producing organisms.

A distal or type 1 RTA is classically associated with a more significant drop in the serum HC0 3 (usually< 12 mEq/L), an elevated urine anion gap, a reduced urine osmolal gap, an elevated urinary pH, the possible presence of renal stones, and a low or normal serum potassium. Causes of a distal RTA are listed in Table 1-8. The diagnosis of a proximal RTA requires a high degree of clinical suspicion, as it cannot be diagnosed based on the urine anion gap or the urine osmolal gap (see Table 1-9). In addition to abnormalities in urinary HC0 3 resorption, patients may have abnormalities in the absorption of other solutes from the proximal tubule ( eg, phosphate, uric acid, amino acids, glucose). This more generalized proximal tubule dysfunction is termed Fanconi syndrome. The urine pH and urine anion/osmolal gap calculations are not helpful unless the patient is receiving a HC03, or the disease process is caught very early. Once the process becomes chronic, the patient reaches a steady state in terms of the serum HC0 3 (12 to 18 mEq/L), and therefore

TABLE 1-8

• Evaluation of non-anion gap acidosis.

Evaluation Strategy

1. History (acute or chronic issues, medications. altered GI anatomy, genetic diseases. etc). Also, is the patient receiving an acid load, such as TPN?

2. Does the patient have chronic renal insufficiency? If so, this alone may be responsible for the non-anion gap acidosis.

3. Calculate urine anion gap and urine osmolal gap. The urine anion gap may be of limited value in patients with severe serum anion gap acidosis, as it may be falsely elevated. Similarly, the urine osmolal gap may be lnapproprlately elevated ln patients with a significant serum osmolal gap (particularly due to mannitol).

4. Note the serum potassium as well as the urine pH.

s. If proximal RTA is suspected, look for evidence of other inappropriate compounds in the urine (amino acids, elevated phosphate, glucosuria), and calculate the fractional resorption of sodium bicarbonate (should be > 1 5%). Also check serum for evidence of dysfunction of the PTH-vltamln D-calclum axis.

Cause of NAGMA

LowSerum Potaalum

GI: Diarrhea, pancreaticoduodenal fistula, urinary intestinal diversion

Renal: Type 1 RTA (distal), type 2 RTA (proximal)

Medications/exposures: Carbonic anhydrase inhibitors, toluene

Other: D-Lactlc acidosis

High (or Normal} Serum Potassium

GI: Elevated ileostomy output

Renal: Type 4 RTA or CKD

Medications: NSAIDs; antibiotics (trimethoprim, pentamldlne); heparin; ACE Inhibitors, ARBs, aldosterone antagonists (spironolactone); acid administration (TPN)

Evaluation of RTA

Severity of metabolic Severe (< 10-12 mEq/L Intermediate Mild (15-20 mEq/L) acidosis, [HC03 ] typically) (12-20 mEq/L)

Associated urine Urinary phosphate, Urine glucose, amino abnormalities calcium increased; acids, phosphate, bone disease often calcium may be present elevated

Urine pH

HIGH(>5.5) Low (acidic), until Low (acidic) serum HC03 level exceeds resorptive abillty of proximal tubule; then becomes alkalotic once reabsorptive threshold ls crossed

Serum K+

Low to normal; should Classically low, although HIGH correct with oral HCO, maybe therapy normal or even high with rare genetic defects; worsens with oral HC03 therapy Renal stones

Type1 RTA
Type2RTA
Type4RTA

TABLE 1-8

• Evaluation of non-anion gap acidosis. (contlnuftll Type1 RTA

Renal tubular defect

Reduced NH4 secretion

Reduced HC03

Reduced WIK+ in distal tubule resorption in proximal exchange in distal tubule and collecting tubules due to decreased aldosterone or aldosterone resistance

Urine anion gap > 10

Urine osmolal gap

Reduced

Negative lnitlally; > 10 then positive when receiving serum HCC,; then negative after therapy

At baseline

Reduced (< 150 mOsm/L) during < 100 mEq/L; unreliable (< 150 mOsm/L) acute acidosis during acidosis during acute acidosis ang/otens/n-convertlng enzyme; ARB, anglotensln receptor blocker; Cl<D, chronic kidney disease; GI, gastrolntestlnal; HCO,. bicarbonate; NSAJD, nonstero/dal anti-Inflammatory drug; PTH, parrithyrold RTA. renaltubular addosls; TPN, total parenteral nutrition.

the urine pH and anion gap will be inconclusive and appropriate for the patient's diet. If the patient is placed on a HC0 3 infusion, and the serum HC0 3 levd surpasses the patient's absorptive capabilities, the urine pH will increase rapidly. Altemativdy, one can calculate the fractional excretion (FE) ofHC03• A value greater than 15% indicates that a proximal RTA is likely.

FE =[Urine HCO;J•Serum Cr Hco3 [Serum HCO;J•Urine Cr

A distal RTA is generally associated with a mild reduction in serum HC03 (-18 to 22 mEq/L), an elevated urine anion gap, a reduced urine osmolal gap, a normal urine pH, and an devated serum potassium level.

Finally, for patients with any type of anion gap acidosis, the serum HC0 3 deficit can also be calculated. While HC0 3 therapy is administered only in severe acidemia in patients with lactic acidosis, serum HC0 3 does have a role in the treatment of certain toxicities and in the management of non-anion gap acidosis. First, one must calculate the HC0 3 space, which can then be used to determine the total HC0 3 deficit.

HCQ; space = [0.4 *( ) ] * Lean Body Weight (in kg)

HCQ; Deficit = HC03 space * HC03 Deficit/L

TABLE 1-9

Causes of renal tubular addosls.

Causes of Type 1 (Distal) RTA

Primary

• Idiopathic or famlllal (may be recessive or dominant)

Secondary

• Medications: Lithium, amphotericin, ifosfamide, NSAIDs

• Rheumatologic disorders: Sj0gren syndrome, SLE. RA

• Hypercalciuria (idiopathic) or associated with vitamin D deficiency or hyperparathyroidism

• Sarcoldosls

• Obstructive uropathy

• Wilson disease

• Rejection of renal transplant allograft

• Toluene toxicity

Causes of Type 2 (Proximal) RTA

Primary

• Idiopathic

• Familial (primarily recessive disorders)

• Genetic Fanconi syndrome, cystinosis, glycogen storage disease (type 1), Wilson disease, galactosemia

Secondary

• Medications: Acetazolamlde, toplramate, amlnoglycoslde antlblotlcs, lfosfamlde, reverse transcriptase inhibitors (tenofovir)

• Heavy metal poisoning: Lead, mercury, copper

• Multiple myeloma or amyloidosis (secondary to light chain toxicity)

• SJ(jgren syndrome

• Vltamln D detlclency

• Rejection of renal transplant allograft

Causes of Type 4 RTA (Hypoaldosteronism or Aldosterone Resistance)

Primary

• Primary adrenal insufficiency

• Inherited dlsorders assoclated with hypoaldosteronlsm

• Pseudohypoaldosteronism (types 1 and 2)

Secondary

• Causes of hyporeninemic hypoaldosteronism such as renal disease (diabetic nephropathy), NSAID use, calcineurin inhibitors, volume expansion/volume overload

• Causes of distal tubule voltage defects such as sickle cell dlsease, obstructive uropathy, SLE

• Severe illness/septic shock

• Angiotensin II-associated medications: ACE inhibitors, ARBs, direct renin inhibitors

• Potassium-sparing diuretics: Spironolactone, amiloride, triarnterene

• Antibiotics: Trlmethoprlm, pentamldtne

ACl;. angiorensin-converting enzyme; ARB. angiotensin receptor blocker; NSAID, nonsteroidal anti-inflammatory drug; RA. rheumatoid arthritis; RTA. renal tubular addosis; SLl;. systemic lupus erythematosus

RESPIRATORY ACIDOSIS

The algorithm for the evaluation ofa respiratory acidosis is shown in Figure 1-4. It is particularlyhelpful to determinewhethera patienthas abaselinerespiratoryacidosis prior to evaluation as it will greatly aid in determining the acute acid-base disorders presentThe first step in the evaluationis to determineifthemetabolic compensation is appropriate. This requires a decision as to whether the respiratory process is acute

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story connected with these ruins which hold so closely the secrets of the past.

CHAPTER III Tyuonyi

Could one be so bold as to say that the Moslem Invasion of Spain in the eighth century A.D. took place after the first occupation of the Rio Grande Valley by prehistoric Indians? Archæologists, who tell us stories based on the remains of things they have found, broken pottery mostly, say that Indians might have known the Rio Grande before this time. We believe that they have occupied it continuously since about the eleventh century A.D.

Drought seems to have always been one of the main controlling factors in the migrations of Southwestern Indians. The study of treerings tells us this. By matching ring patterns formed by the annual growth of certain kinds of trees, pines chiefly, archæologists are able to determine the years in which age-old timbers were cut. Those they are interested in are the ones used by prehistoric Indians long years ago for building roofs on their houses. So naturally, if an Indian had cut a tree down with a stone axe and laid it across the walls of his house, then the year that the tree was cut would correspond to the approximate time his house was built and occupied. Indians did not cut timbers until they were ready to use them. Felling timbers with crude stone axes was somewhat of a chore. Old beams from houses show that long periods of drought reigned in the Southwest. It is thought that these dry spells caused Indian families to leave their homes and seek new lands for settlement and cultivation.

Such a condition seems to have existed in the entire San Juan area of northwestern New Mexico, northeastern Arizona and southwestern Colorado. The greatest of the large centers of Indian population, which may have numbered hundreds or even

thousands of people, were the towns of Chaco Canyon in northwestern New Mexico and the Mesa Verde cliff dwellings in southwestern Colorado. Many of these towns, it seems, were abandoned when the great drought was at its height between 12761299, a period of twenty-three years. And so we find shifts in population. It is believed that some of these shifts were toward the Valley of the Rio Grande.

Before this time small individual groups or migrant bands took to wandering. Other Indians could have remained even after the time of the twenty-three year drought period, dreading to leave their homes as we would ours today. No, there was no great exodus of population. The people from the great towns in the west did not move out all at one time and completely abandon their homes and desiccated lands. They moved out in small bands, or even families. In some way, a traveler might have reported high mountain ranges, water and fertile lands to the east—the next best to the places they knew as home which they and their ancestors had occupied for hundreds of years.

It is possible that even in the 1000’s A.D., small groups pushed out over dry desert wastes, following sandy arroyo beds—thought of water ever paramount. They were people struggling again for existence. Some likely stopped along the way and built temporary homes. They broke pottery vessels which they had brought along. The archæologist found some of the broken pieces nine hundred years later to help tell the story. Whether these migrant bands had a goal or not is questionable but the Valley of the Rio Grande was finally reached and scant evidence of these early people has been found. More and more Indians moved out of the San Juan area and drifted in a southeasterly direction. Some clung to the valleys, others took to the mountains, but all settled in the general locality where we find most of our colorful and picturesque Indian Pueblos so well-known the world over—northern New Mexico.

20

It is evident that by constant roaming, and penetrating unknown and fascinating country, some of these primitive Indians stumbled into the deep valleys and upon the high forested mesa tops of the Pajarito Plateau, about twenty miles west of the present city of Santa Fe. The spot on which Santa Fe is located was then nothing but arid mesa land and low foothills ascending to the Sangre de Cristo Range of Mountains. Four things were paramount in the minds of these primitive people. They were water, food, protective shelter and clothing. These were the things the Pajarito offered. Anyone journeying through the deep canyons and over the high mesa tops today could easily see why prehistoric Indians settled here.

For centuries the wind pounded tiny sharp particles against cliff surfaces. It whipped up close to the ground and hollowed out shallow caves. Very likely, these places were not large enough for Indians to crawl in out of the weather but the cliff composition was so soft that these natural caves could easily be made larger. A crude stone of basalt with a sharp edge made a perfect hand axe. Indian men hacked out caves large enough for a little family group to enter. Rain and cold created the necessity for heat. Drills of wood were used to start fires in these crude cave dwellings. Fires made them warm— suffocatingly so. There was no way for the smoke to escape except through a wide front opening. This lack of ventilation created a very serious problem for the early cave dweller on the Pajarito Plateau.

There were other Indians who preferred to build their homes on the high mesas during these early times. Adobe was used almost exclusively to build the low walls of rooms. Some bedded small stones into the walls before they were dry. This helped to hold them together. Others preferred to use larger stone, picked up at random, in building their house walls. The adobe huts were undoubtedly unsatisfactory because of their low resistance to weather. Since older styles of pottery have been found in the ruins of these houses, it is logical to suppose that Indians migrating onto the Pajarito built adobe houses first. Later they dug themselves out homes in the cliffs

22 which gave them greater protection from the weather and from any invaders.

In this wilderness a mule deer could have fed in a little valley or drunk from a creek. This would mean food for the entire family or group if a crude arrow would hit its mark. Small razor-sharp fleshers of chalcedony or basalt were used to remove the hide from the carcass. The hide could be used for making clothing or moccasins. Some of the smaller bones might have been used as drills and awls until better ones could be obtained. A flock of wild turkeys would have solved this problem. Turkey bones made excellent awls. Just what the people used for arrow points during these early times is questionable. Maybe they brought them along from the west. They could have used chipped chalcedony or basalt which was readily found, and quite common in this area. An occasional nodule of black volcanic glass, called obsidian, washed down the creek and was found bedded in its soft sandy bottom. Obsidian might have been more popular during later times as the early dweller in this country may not have discovered the ledges of black glass immediately upon his arrival. Such could have been life on the Pajarito Plateau eight hundred years ago.

More groups of people came in. Hand-hewn caves could have dotted the soft workable walls of every canyon which would support human life. The well-known canyon of today, the Frijoles, was one such place. The lower part of the valley formed a sort of a bulb for about two miles. Its sheer cliffs on the north side rose to terrific heights. And throughout the countless years, as boulders and dust fell from the cliffs, a talus slope or base had formed. A little river, the Rito de Los Frijoles, ran for seventeen miles from its source in the high mountains to the west and emptied into the Rio Grande. This Canyon was the best in the entire Pajarito—the most coveted of all habitable places. The water supply was apparently constant and the valley was broad and open at the lower end, most suitable for agriculture. The floor was densely covered with growths of scrub oak, piñon and pine. This was all that primitive groups needed for

successful living. And so we find that some of these wandering Indians from a world a hundred miles to the west, which was to become a thing of the past, penetrated the Valley of the Frijoles over eight hundred years ago. But Frijoles Canyon was not the only place occupied. There were other canyons nearby. There was plenty of room for all. But was there enough water in these other canyons?

Indian families cut their crude shelters deep enough for occupation by several individuals. Caves were uncomfortable, but certainly better than no shelter at all. This was a strange sort of stone which nature had provided. It was very poor to build with, thought the Indian. It was soft and bulky. But years of living would eventually solve the problem. Why worry about it! In time necessity would produce some means of shelter more satisfactory. Later on, more people moved into the area. These people occupied adjacent canyons and mesas as well as Frijoles. During many years population increased and the dwellers on the Pajarito became settled in their locality.

There is no way of telling how many Indians lived in the Valley of the Frijoles during very early times—close to water and well protected. Indians could sit at the openings of their cave homes above the talus slope and see for great distances up and down the Canyon. And it was safe. No jealous enemy lurking above could roll a boulder down on them. Their cave was their protection. But caves were not adequate as homes. Fires could not be built inside without smoking out its occupants. Something better had to replace them. This new soft rock certainly was not suitable for building walls or at least these simple valley folk did not know how to use it. Crude mud huts were erected at the base of the cliff at the same time that caves were occupied as home sites. Mud was all they could find for building walls. It took lots of water to make mud and then it was so soft and crumbly that the little walls cracked and fell when they dried out.

Soon it was found that by picking up small stones and packing them into the soft mud as temper the walls would stand longer. Larger rocks and less mud made better walls and saved a lot of toil and

unnecessary labor. There were many rocks to be picked up at random. Walls were raised high enough for the Indian to stand upright inside the rooms. Sharp stone axes of basalt were used to fell small trees which were laid over the tops of walls for the support of the roofs. The blunt ends of the timbers were inserted in holes gouged out of the cliff. Brush and grass were placed over them; thick mud coats were smeared over the top. Holes were cut in the roofs. Fires were built and the smoke could escape through these holes. How much better this than a cave! These tiny rooms were stuffy and smoky inside but not as unpleasant as a cave room. An Indian would soon suffocate inside a cave. During the rainy seasons the roofs leaked and great quantities of mud were stirred up and spread over the top and smoothed down flat. The women could always find more when that washed off. In time weeds and wild grasses took root in these dirt roofs.

But somewhere, somehow, not at Tyuonyi perhaps, but in some nearby valley or on some high mesa top at one of a hundred colony sites, Indian neighbors found that still larger chunks of tuff could be used for building blocks. This would save much labor. So much mud in a wall would not be necessary. It is possible that this use of larger building stones was not a matter of independent origin at any one of many primitive villages on the high mesas and in the deep canyons of the Pajarito. Indians, after years and years of living, simply came into the use of larger building blocks by the trial and error method. They served the purpose better. A dry spell or so, when it did not rain, might have made it necessary to transport more and more water in urns from water holes or nearby streams. This was women’s work and hard work too. And more stone and less mud made stronger walls for houses anyway. Some of the stone was so soft that it could be shaped into blocks to fit into the walls. These blocks did not lay absolutely flat because their surfaces were irregular. Small stones were forced between the cracks and when the mud mortar dried the walls were solid. This practice went on for years and years. Indians experimented with all the materials at their

24

Everywhere on the Pajarito are seen the remains of homes belonging to this period of occupation. There are hundreds of them—small family houses, in deep canyons or in a forest on high mesa tops. Debris has filled them up and today they look like piles of rock. Building blocks are strewn all over the surface. Most of the blocks had been picked up at random after they had been carved by nature. Others were square or rectangular, showing that they had been fashioned by Indian hands.

The Indians who lived in the Valley of the Frijoles communicated with the other groups who lived in deep canyons to the south and to the north. They visited each other and even traded back and forth. Little colonies were formed when one, two, three or four families lived together in a house with several rooms. But the time was to come when this living all over the country would stop; people would come together to live in communities. And the little colony sites would be abandoned forever for the archæologist to discover centuries later.

25 disposal. They could not send an order to the Gods for building materials.

A touchy subject is that of linguistics. It is a tricky one. But students know that five different languages are spoken among the Pueblo Indians of New Mexico today. They are: Tiwa, Tewa, Towa, Keres, and Zuñian. To be on the safe side, one should not touch too heavily upon languages spoken by Indians, especially in a writing of this kind. But languages and dialects do play an important part in our story. When those early people drifted from Chaco Canyon and Mesa Verde toward the Rio Grande, they spoke a language. But, it is unknown. Students have ideas, but are reluctant to advance opinions based on the ruins they excavate or the artifacts they discover. But, two groups of Indians speaking different languages drifted onto the Pajarito. People speaking different languages have never gotten along well together even from the Tower of Babel until the present time.

It has been mentioned before that Keres-speaking Indians have a legend that long years ago a treaty or contract was made between their ancestors and Tewa-speaking people. It is said that certain loosely defined ranges of territory were to belong to each of the two groups. The meeting place or the place where the treaty was made was called “Tyuonyi.” “Tyuonyi” means “place of treaty.” Thus the dividing line between Tewa and Keres lands became sharply defined by what is now known as “Frijoles Canyon.” But how long was such a treaty to last among primitive people? All the lands to the south of Frijoles Canyon were supposedly Keres and those to the north were Tewa. After this treaty was made, Indians probably spread out on each side of the Canyon like the parting of the waters of the Red Sea. Small house sites dotted the mesas and canyons on both sides. But still, members of both groups could possibly have lived here together.

Legend hints at this.

As time went on more houses sprang up at the base of the north cliff and crude pueblos were erected on the floor of the Canyon. Kivas or ceremonial chambers were dug out of the valley floor and lined with walls of rock. Indians gathered cobble stone because they might not have known how to cut blocks during these early times with which to lay masonry walls. They gathered thousands of them and built their kiva walls eight or ten feet thick. This was their attempt to utilize the pieces of crudely shaped felsite or volcanic ash. They laid huge timbers fifteen or more inches in diameter across the walls of their large underground chambers. Then smaller poles of pine were cut and laid on top of the large vigas. Splittings were hacked from down trees. Pine, cottonwood, juniper, piñon anything that would split easily with crude stone implements—were used for the next roof course. Then brush and grass and mud were put on top. The roofs must have been two or more feet thick but little did the Indians realize that the tremendous weight might crack the big timbers after they dried out. How ingenious were these Indians in their simple way!

26

Many a moon passed. Many houses were built. Jealousy might have arisen between these two groups of Indians. Who was to raise corn on this or that little patch of fertile ground? Who should have a right to hunt deer and turkey in the Valley of the Frijoles? How could Keres-speaking people go to Tewa kivas or how could Tewas go to Keres kivas? Trouble reigned over the entire plateau and most of it was possibly in the Valley of the Frijoles. Was it ever decided which group should live in Hidden Valley when it was given the name Tyuonyi?

Jealousy could have arisen over pottery. When the Frijoles area was first occupied clay deposits were discovered in arroyos and along river banks. Indian women began moulding pottery with local clays. They discovered mineral pigments. They used paints from wild plants which fired the black designs in fast color in the vessels. The color would never come out. But slowly and surely the women began to depart from the techniques which they and their ancestors had previously used. Out of these techniques new styles of pottery were developed by using local materials. These white wares with black designs became thick and coarse as time went on and probably decreased in popularity as far as usefulness was concerned.

27

The Keres-speaking people had kin far to the south of the Pajarito Plateau. And these people were ingenious. Sometime in the thirteenth century, it seems, Indians living in the Little Colorado River district of what is now eastern Arizona and western New Mexico, were making a style of red pottery with black designs. This pottery was apparently very popular and spread by trade to the Rio Grande Valley. Indians in this same region eventually learned to produce a glaze paint by using lead-manganese ore. This ware also spread to the Rio Grande and glaze paint was used in decorating pottery from about 1350 A.D. to the time of the Pueblo Rebellion in 1680. It is thought that shortly after its inception and perhaps by 1400 A.D. this red pottery spread by trade to Tyuonyi.

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