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MultidimensionalAnalytical TechniquesinEnvironmental Research

Multidimensional AnalyticalTechniques inEnvironmental Research

Elsevier

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Contributors

AntoineS.Almeida DepartmentofChemistry&CESAM,UniversityofAveiro, Aveiro,Portugal

PedroF.Branda ˜ o DepartmentofChemistry&CESAM,UniversityofAveiro, Aveiro,Portugal

Marie-CecileChalbot NewYorkCityCollegeofTechnology,BiologicalSciences Department,Brooklyn,NY,UnitedStates

XiChen AnhuiProvinceKeyLaboratoryofFarmlandEcologicalConservationand PollutionPrevention,SchoolofResourcesandEnvironment,AnhuiAgricultural University,Hefei,China

WenyingChu DepartmentofChemistryandBiochemistry,OldDominion University,Norfolk,VA,UnitedStates

ArmandoC.Duarte DepartmentofChemistry&CESAM,UniversityofAveiro, Aveiro,Portugal

ReginaM.B.O.Duarte DepartmentofChemistry&CESAM,UniversityofAveiro, Aveiro,Portugal

HongjianGao AnhuiProvinceKeyLaboratoryofFarmlandEcologicalConservation andPollutionPrevention,SchoolofResourcesandEnvironment,AnhuiAgricultural University,Hefei,China

JeffreyA.Hawkes UppsalaUniversity,Uppsala,Sweden

DeanHesterberg DepartmentofCropandSoilSciences,NorthCarolinaState University,Raleigh,NC,UnitedStates

IliasKavouras CUNYGraduateSchoolofPublicHealth&HealthPolicy, DepartmentofEnvironmental,OccupationalandGeospatialHealthSciences,New York,NY,UnitedStates

WilliamKew EnvironmentalMolecularSciencesLaboratory,PacificNorthwest NationalLaboratory,Richland,WA,UnitedStates

JingdongMao DepartmentofChemistryandBiochemistry,OldDominion University,Norfolk,VA,UnitedStates

Ca ´ tiaMartins DepartmentofChemistry&QOPNA/LAQV-REQUIMTE,University ofAveiro,Aveiro,Portugal

MauroMecozzi LaboratoryofChemometricsandEnvironmentalApplications, ISPRA,Rome,Italy

JenniferMejia DepartmentofChemistryandBiochemistry,OldDominion University,Norfolk,VA,UnitedStates

CarinaPedrosaCosta DepartmentofChemistry&QOPNA/LAQV-REQUIMTE, UniversityofAveiro,Aveiro,Portugal

Sı´lviaM.Rocha DepartmentofChemistry&QOPNA/LAQV-REQUIMTE, UniversityofAveiro,Aveiro,Portugal

YingxinShang NortheastInstituteofGeographyandAgroecology,Chinese AcademyofSciences,Changchun;UniversityofChineseAcademyofSciences, Beijing,China

AakritiSharma DepartmentofCropandSoilSciences,NorthCarolinaState University,Raleigh,NC,UnitedStates

KaishanSong NortheastInstituteofGeographyandAgroecology,ChineseAcademy ofSciences,Changchun,China

SophiaViar 2505TiswoodCourt,Chesapeake,VA,UnitedStates

ZhidanWen NortheastInstituteofGeographyandAgroecology,ChineseAcademy ofSciences,Changchun,China

YingZhao NortheastInstituteofGeographyandAgroecology,ChineseAcademy ofSciences,Changchun,China

Multidimensionalanalytical techniquesinenvironmental research:Evolutionofconcepts

Challengesinenvironmentalresearch

1

Nowadays,mostoftheenvironmentalchallengesareassociatedwiththeincreased releaseofpollutantsintotheair,water,andsoil,modificationsontheglobalcycling ofnutrientsandcontaminants,andclimatechangeissues.Theadvancementsmade thusfarinenvironmentalresearchhaveoriginatedeitherfromtheneedtounderstand theabovementionedissuesortoseeksolutionsandregulations.Eitherway,moststudiesfocusonunderstandingtheinteractionswithinandamongatmospheric,terrestrial, aquatic,andlivingcompartmentsofecosystems.Thisis,however,anextremelychallengingtask,mainlyduetothevariabilityofthoseecosystemsandthehighdegreeof heterogeneity,bothintermsofcompositionandconcentration,ofthesamplesand analytesofinteresttakenfromthedifferentenvironmentalcompartments.Thiscomplexityrepresentsatrueanalyticalchallenge.Itis,therefore,notsurprisingthatthe developmentofnewanalyticalstrategiestounravelsuchcomplexmatriceshasoccupiedacentralroleintheeffortofresearchers.

Thedramaticdevelopmentduringthepastdecadeinadiversesuiteofanalytical tools,usingasecondorthirddimensionormultiscalehyphenatedmethods(i.e.,separativeanddetectionmethods),havecontributedtoadvancesinenvironmental research.Theseadvancesincludesignificantimprovementsin(i)analyticalsensitivity andaccuracyforthetargeted,semitargeted,anduntargetedscreeningofcomplex organicmatrices(e.g.,high-resolutionmassspectrometry,HR-MS [1–6]);(ii)the useand/orcombinationofspectroscopic[e.g.,one-andtwo-dimensional(2D) liquid-andsolid-statenuclearmagneticresonance(NMR)spectroscopy [7–12], andexcitation-emissionmatrix(EEM)fluorescencespectroscopy [13–16]],HR-MS [17–20],andchromatographicseparation(e.g.,Ref. [21])toacquirecompositional, geographic,andtimeevolutioninformationoncomplexorganicstructuresandinteractions;(iii)developmentofpowerfulcomprehensivemultidimensionalchromatographictoolsfortheresolutionofcomplexorganicmatrices(e.g.,Refs. [22–30]); (iv)useofsynchrotronradiation-basedmethodstoelucidatethespeciationandspatial arrangementoftoxicelementsandnutrientsincomplexenvironmentalmatrices(e.g., Refs. [31–36]);and(v)developmentofmore“user-friendly”dataprocessingand treatmentsoftwaretodealwiththecomplexityofmultidimensionaldatagathered

2 MultidimensionalAnalyticalTechniquesinEnvironmentalResearch

fromtheenvironmentalsamplesinordertogleanthedesiredinformation(e.g.,Refs. [37,38]),tonameafewofthemany.Thecomplementarityandtechnological advancesofthesemultidimensionalanalyticaltoolshavebeenkeytoallowawider rangeofcomplexenvironmentalmatricestobeanalyzed,enablingtheacquisitionof innovativedataandtransformativeadvancesinenvironmentalresearch.

Thischapteraimstointroducethereadertotheunderlyingconceptsthathave driventhedevelopmentanduseofsophisticatedmultidimensionalandmultiscale hyphenatedmethodsforunravelingcomplexorganicmixturesfromdifferentenvironmentalmatrices.Thefocusisonsecond-andthird-dimensionalspectroscopic, spectrometry,andchromatographicmethods,andhowthesestate-of-the-artmultidimensionalanalyticalstrategiesarebeingusedforthetargetedanduntargeted profilingofsuchcomplexorganicmixtures.Thisisnotacomprehensivereviewon theuseoftheseanalyticalmethodologiesbutinsteadabroadoverviewandan introductiontothesubsequentchapters,wherethemostpopularmultidimensional analyticaltechniquesusedinenvironmentalbiogeochemistryresearcharecarefully addressed.

Copingwithenvironmentalorganicmatricescomplexity

Inrecentyears,therehasbeenanincreasingconcernforenvironmentalmonitoringand developmentofnewanalyticalproceduresfordealingwiththehugenumberofanalytes andtacklingthegreatcomplexityofenvironmentalsamples.Thesecomplexorganic mixturesexhibitadiversityofconstituentswithdifferentmolecularsizes,structures, andchemicalproperties,whichmakestheiranalysisoneoftheenduringchallenges inanalyticalchemistry.Forexample,whilesolvingthechemicalstructureofhigh molecularsizeanalytes,suchasproteinsorothernaturalpolymers,requiresexploring therelativelywell-organizedcompositionoftheirsmallermolecularsubunits (i.e.,monomers),theanalysisofsmallermoleculesinamixtureisrathermoredifficult. Inthelattersituation,theanalystfacesabroadchemicalandstructuraldiversity,which requiresdifferenttypesofanalysesifaimingatthefullstructuralidentificationofeach organiccompound[i.e.,elementalcomposition,spatialstructure(i.e.,itsisomers), and/orspatialconfiguration].Nevertheless,notallenvironmentalproblemsrequire thefullidentificationofallorganiccompoundspresentinasample. Fig.1.1 illustrates howdifferentlevelsofcompositionalinformationcanbedistinguished,depending onthepurposeofinvestigation:(i)functionalgroupanalysis,whichcopeswith thehighestlevelofmoleculardiversity(numberoforganiccompounds, n 1000)at theexpensesofchemicalresolution,istypicallyemployedwheninterestedinunderstandingspecificpropertiesofcomplexorganicassemblies(e.g.,structuralaverage information [7,8,10,12],chemicalprocesses [9,39],opticalproperties [13,40], andfine-scalespatialarrangementoforganiccarbonforms [31,34,35]);(ii)resolve thechemicalcompositionofcomplexorganicmixturesintodifferentorganic componentsormolecularstructures(10 n 100)isusuallychosentounraveling themolecularcodes [11,21,41–45],theorganicprecursors [20,46,47],andreactivity [1,48,49] ofthesehighlycomplexmixtures;(iii)targetanalysisofmolecularorganic

Fig.1.1 Levelsoforganiccompositionalidentificationintheanalysisofcomplexmixtures fromdiverseenvironmentalmatrices,highlightingthequantificationattainedbydifferent advancedanalyticaltechniques(n:numberoforganiccompoundsidentifiedand/ormeasured).

markers(n 10)istypicallyusedtoaccuratelyquantitateand/ormonitoringknown formationprocessesorsourcesofthetargetcompoundsindifferentenvironmental matrices [23,24,28,29,50–54];and(iv)correspondingtothehighestlevelofchemical resolution,theidentificationofuptothreespecificorganiccompounds(n 2–3)when studying,forexample,unknownformationprocessesorsourcesoforganicparticlesin theatmosphere(Ref. [55] andreferencestherein)oridentifyingemergingorganic pollutantsinindustrialwastewater [56] orfreshwater [57].

Inenvironmentalresearch,theaimoftheanalysisandthechoiceofafitforpurpose analyticalmethodologyarestronglyinterconnectedandshouldbethoroughly assessedbeforehand.Identifyingspecificorganiccompounds(knownorunknown) inacomplexenvironmentalsample(i.e., n 10in Fig.1.1,suchastheidentification andquantificationoforganicpollutantsinawatersample)isdifferentfromaglobal characterizationofthewholeenvironmentalsample[i.e., n 1000in Fig.1.1,suchas thecharacterizationofnaturalorganicmatter(NOM)].Regardlessofusingatargeted oruntargetedanalyticalapproach,akeyobjectiveofanalyticalchemistryhasbeenthe continuousimprovementanddevelopmentofanalyticalmethodologiescapableof reducingacomplexproblemintomanageabledatasets.Astheenvironmentalproblemscontinuetogrowevermorechallenging,thelevelofcompositionalidentification hasevolvedtowardtheintegrationofdifferentanalyticaldimensionstoreachtheresolutionnecessaryforthedetectionandidentificationofabroaderrangeofmolecular structures.Thefollowingsectionsintendtohighlightthosemultidimensionalanalyticalapproachesthatcanenticetheresearcherstocopewiththecomplexityofenvironmentalsamplesand,thus,discoveryetunknownnewmolecules.

Multidimensionalnuclearmagneticresonance(NMR) spectroscopyinenvironmentalresearch

NMRspectroscopyhasunquestionablemeritsinthestructureelucidationoforganic structuresincomplexmixtures.Thehighreproducibility,aswellasthenondestructive andnoninvasivecharacteristicsofNMRspectroscopyarekeyadvantagesforemploying thistechniqueinenvironmentalresearch.NMRcanbeappliedforin-depthstudiesof mostenvironmentalmatrices,includingliquid,gels,andsolidsamples,orevenforthe elucidationoforganicstructurespresentinallphasesinunalteredenvironmental samples [58].ThisfeatureofNMRreliesonthedifferenttechniquesavailable,thus makingNMRspectroscopyapivotalanalyticaltooltounravelthecomplexityofthe countlessmolecularstructurestypicallyfoundinvariousenvironmentalsamples (Fig.1.2).TheNMRtechniquesavailableincludesolution-stateNMR,solid-state NMR,gel-phaseNMR,andcomprehensivemultiphase(CMP)NMRspectroscopy. Foramorein-depthdiscussionofallthesetechniques,experimentalprotocols,and applicationsintheanalysisofenvironmentalcomplexmatrices,thereaderisencouragedtorefertothereviewworksofSimpsonetal. [7,59],Maoetal. [8],andDuarte andDuarte [10],aswellasto Chapters2 and 3.Here,itisintendedtohighlightthe advantageofusingtheseNMRtechniques,particularly2DNMR,toacquireawealth ofinformationonthemolecularbonds,structures,andinteractionswithinthecomplex organicfractionpresentinwater,soils,sediments,andairparticles.

Solution-stateNMRspectroscopyinenvironmentalresearch

Solution-stateNMRisideallysuitedtoacquirecomprehensivemolecularinformationof complexorganicmatricesthatarenaturallysoluble,suchasthedissolvedorganic matter(DOM)fromice [60] andwater [20,61],butalsotheorganicmatterisolated fromsoils [7] andairparticles [11,62–64].Undoubtedly,solution-stateone-dimensional (1D) 1HNMRtechniquehasaprimepositionasatoolforrapidscreeningand determinationofthegeneralstructuralpropertiesofsuchcomplexorganicmixtures. Althoughprovidingarelativelybroad1DprofileofDOM,onecanstillwithdraw excellentcompositionalinformationonthesample,includingnear-quantitative dataonthedifferent 1HfunctionalgroupswithC-Hbonds,aslongasthespectraarecarefullyacquired,processed,andinterpreted.Thesesemiquantitativeapproacheshavebeen used,forexample,toassessthemoleculardivergencewithinDOMfromdifferent wetlands [61] ortoshedlightonthedominantsourcesofatmosphericorganicaerosols atdifferentlocations(i.e.,sourceapportionment) [65].Thewell-knowndownsideof solution-state1D 1HNMRofcomplexorganicmatricesisthataccuratequalitative andquantitativestructuralassessmentishamperedbythehighdegreeofoverlap characterizingthesespectra.Threemainreasonscanexplainthisspectraloverlap: (1)theresonancesaredispersedoveralimited 1Hchemicalshiftrange (δH 0–10ppm),(2)thepresenceoforganiccompoundswithresemblingstructural features,forwhichthecorresponding 1HNMRspectraareverysimilar,and(3)the presenceofahighnumberofcompoundsresonatinginthesamelimitedspectralregion.

Fig1.2 Seefigurelegendsonnextpage

Oneappealingsolutiontoovercomethespectraloverlappingissueistorelyon solution-statemultidimensionalNMRspectroscopy.Themultidimensionalapproach hasthehighadvantageofofferingamuchbetterdiscriminationofresonances than1DNMRasthepeaksarespreadalongasecondorthirddimension(1Hor 13C frequencies),thusenhancingthereliabilityofNMRassignmentsandallowthe identificationofmolecularfragments,viahomonuclear(1H-1H)andheteronuclear (1H-13C)connectivityinformation [7,66].Undoubtedly,themostimportantmultidimensionalsolution-stateNMRexperimentsappliedintoenvironmentalresearch arethe2DNMRtechniques,including(a) 1H-1HhomonuclearCOSYandTOCSY, whichprovideconnectivityinformationbetweenprotonsthataredirectlyattachedto adjacentcarbons(COSY),orregardingagivenprotonthatisinteractingwithother protonsofthesamestructurewhicharewithinthespinsystem(unbrokenchainof couplings)oftheatom(TOCSY);(b) 1H-13CHSQC,whichdetectsH-Ccouplings overonebondandprovideschemicalshiftdataforbothatomsinaC-Hunit; and(c) 1H-13CHMBC,whichprovidesdirectevidenceaboutthebondingofH-C fragmentsovertwo-andthree-bondrange(i.e.,H-C-C orH-C-C-C) [67].The combinationof 1H-1Hhomonuclear(COSYand/orTOCSY)with 1H-13Cheteronuclear (HSQCandHMBC)connectivityinformationisapowerfulapproachforassignmentof signals,allowingahigherspectralresolutionand,therefore,greaterdetailontheC-H backboneofthesubstructurespresentincomplexorganicmatricessuchasthoseof NOM [7,11,20,61–63,65,68].Recently,anisotope-filtered nDNMR methodology—acombinationofisotopictaggingand nDNMR—wasdevelopedto characterizephenolicmoietiesofhumicmolecules [69].Theprinciplewasillustrated

Fig.1.2 Solution-state,solid-state,andcomprehensivemultiphaseNMRspectroscopy employedinthestructuralcharacterizationofdifferentenvironmentalmatrices. Reprinted(adapted)withpermissionfromJ.T.V.Matos,R.M.B.O.Duarte,S.P.Lopes, A.M.S.Silva,A.C.Duarte,Persistenceofurbanorganicaerosolscomposition:decodingtheir structuralcomplexityandseasonalvariability,Environ.Pollut.231(2017)281–90, https://doi. org/10.1016/j.envpol.2017.08.022 (Copyright(2017),withpermissionfromElsevier),R.M.B.O. Duarte,S.M.S.C.Freire,A.C.Duarte,Investigatingthewater-solubleorganicfunctionalityof urbanaerosolsusingtwo-dimensionalcorrelationofsolid-state13CNMRandFTIRspectraldata, Atmos.Environ.116(2015)245–52, https://doi.org/10.1016/j.atmosenv.2015.06.043 (Copyright (2015),withpermissionfromElsevier),X.Cao,G.R.Aiken,R.G.M.Spencer,K.Butler,J. Mao,K.Schmidt-Rohr,NovelinsightsfromNMRspectroscopyintoseasonalchangesinthe compositionofdissolvedorganicmatterexportedtotheBeringSeabytheYukonRiver, Geochim.Cosmochim.Acta181(2016)72–88. https://doi.org/10.1016/j.gca.2016.02.029 (Copyright(2016),withpermissionfromElsevier),D.Courtier-Murias,H.Farooq,H. Masoom,A.Botana,R.Soong,J.G.Longstaffe,etal.,ComprehensivemultiphaseNMR spectroscopy:basicexperimentalapproachestodifferentiatephasesinheterogeneoussamples,J. Magn.Reson.217(2012)61–76, https://doi.org/10.1016/j.jmr.2012.02.009 (Copyright(2012), withpermissionfromElsevier),andM.TabatabaeiAnaraki,R.DuttaMajumdar,N.Wagner,R. Soong,V.Kovacevic,E.J.Reiner,etal.,Developmentandapplicationofalow-volumeflow systemforsolution-stateinVivoNMR,Anal.Chem.90(2018)7912–21, https://doi.org/10.1021/ acs.analchem.8b00370 (Copyright(2018)AmericanChemicalSociety).

usinga4D 13CH3O-filteredNMRexperiment,whichcorrelateschemicalshiftsoffour nuclei—thearomaticCHatoms ortho tomethoxygroupsandthoseof 13CH3Oatoms. Theinformationgatheredonthemultiplechemicalshiftsandcouplingconstantshave ledtotheidentificationofthemajorsubstitutionpatternsofninephenolicaromaticmoietiesofapeatsoilfulvicacid [69],andtheprospectofapplyingothertagscontaining NMR-activenuclei(e.g.,suchas 15Nand 31P).

Regardlessofthesolution-statemultidimensionalNMRexperimentemployedin thestructuralcharacterizationofcomplexorganicmixtures,itisadvantageousto extract/isolate/preconcentratetheorganiccomponentfromtheoriginalenvironmental matrix,particularlywhendealingwithwater,soil,orsedimentsamples.Theoutcome ofthepreprocessingsampleprocedureistwofold:(1)itdecreasestheheterogeneityof thesample,byenrichingtheisolatedfractionsinthoseorganicspeciesthatare targetedbythephysicochemicalmechanismsgoverningtheirextraction,and(2) removestheparamagneticspeciesthatinterferewithNMRsignalacquisition,thus enhancingboththesensitivityandresolutionofthespectra.Analternativewayof improvingNMRdetectionofuniquemolecularstructureswithincomplexorganic mixtures,suchasthoseofnaturalorganicmatter,isthroughthechromatographic separationofthesematricesintosimplifiedfractionspriortoofflineNMRdetection. AsshownbyWoodsetal. [21,45],improveddiscretestructuralassignmentswithin DOMarereadilyattainableusingmultidimensional[1D,2D,andthree-dimensional (3D)]NMRforthecharacterizationofsimplifiedchromatographicDOMfractions. MultidimensionalNMRdataprovidedarangeofconnectivityandchemicalshift informationthatisnotapparentfromtheunfractionatedDOMmaterial [21,45] Ithasbeenalsoshownthatsolution-statemultidimensionalNMRcanbeusedto characterizecomplexenvironmentalsampleswithlimited[e.g.,water-solubleorganic matter(WSOM)fromatmosphericaerosols [62]]orevenwithnopreconcentration procedure(e.g.,DOMfromice [60],aswellasrivers,lakes,andtheocean [70–72]).Theapplicationofimprovedwatersuppressiontechniqueshasallowed theacquisitionofmeaningfulNMRspectraandthesubsequentcharacterization oftheorganicmatteratitsnaturalabundanceinalmostunalteredenvironmentalsamples.Althoughprovidingcompositionalinformationontheorganicconstituentswithoutpretreatment,thesestructuraldataareacquiredattheexpensesoflongtimesof analysis,whichusuallypreventstheapplicationofthisprocedureonaroutinebasis.

Solid-stateNMRspectroscopyinenvironmentalresearch

Solid-stateNMRistraditionallyperformedondriedsamples(100–500mgofsample massisrequired)andalsowidelyemployedtoinvestigatethestructureofNOMfrom diverseenvironmentalmatrices.Inthisregard,thereaderisencouragedtorefertothe reviewworksofMaoetal. [8],Cook [73],andDuarteetal. [10] ontheapplicationof solid-stateNMRspectroscopytoNOMstudiesfromwater,soils,andatmospheric particulateorganicmatter.Inasimilarwaytosolution-stateNMR,high-quality solid-stateNMRdataofenvironmentalsamplescanbeobtainedifconcentrating theorganicmatterbyremovingtheparamagneticspeciesfromthecomplexmatrix, typicallybyusingasolid-phaseextractionprocedure.

13Cisthemostcommonlydetectednucleusinsolid-stateNMRofenvironmental samples.Duetothelownaturalabundanceand,therefore,lowsensitivityof 13Cdetection,cross-polarization(CP)incombinationwithmagicanglespinning(MAS)is oftenusedtoenhancethe 13Csignal.DuringCP,themagnetizationispassedfrom protontocarbonforenhancingthesignal;however,thisfeatureisalsothemaindrawbackofCP-MAS,sinceitdoesnotdetectnonprotonatedcarbons(e.g.,carbonatoms ofcarboxylicgroups,orcarbonfromfusedaromaticrings)ormobilesegmentswith weakH–Cdipolarcouplings [74].Toachieveaquantitativeassessmentofallcarbon functionalgroupspresentinasample,directpolarization(DP)combinedwithMAS shouldbeperformed [75].However,theacquisitionofasolid-state 13CDP-MAS NMRspectrumismoretime-consumingthanthatofaCP-MASspectrum.Recently, anewmethodhasbeendevelopedthatyieldsquantitativesolid-stateMAS 13CNMR spectraoforganicmaterialswithgoodsignal-to-noiseratios.Themultiplecrosspolarization(multiCP)techniquedevelopedbyJohnsonandSchmidt-Rohr [74] providesquantitativeinformationaboutallcarbonatoms,typicallyreducingthemeasuringtimebymorethanafactorof50comparedtoquantitative 13CDP/MAS [74]. Thesolid-statemultiCP 13CNMRtechniqueaidbytheapplicationofsuitably designedradiofrequencypulsesequencesallowstargetingsubspectraofspecific typesoffunctionalgroups,suchassp3-hybridizedonly,nonprotonatedcarbons (e.g.,aromaticC-C,andanomericO-C-OandanomericO-C(R,R0 )-Ogroups),mobile CH3 groups,OCH3,immobileCHn-only(i.e.,CH2 andCH),CH2-only,andCH-only carbonsinNOMfromvariousorigins [48,75,76].Thecombinationofdifferent spectral-editingtechniques,whichhavebeendescribedindetailbyMaoetal. [8], couldallowtheidentificationofatleast27differentfunctionalgroupsin 13C NMRspectraofcomplexNOM,incontrasttolessthan10typicallydistinguished intheliteraturebasedonsimple,routine 13CCP-MASNMRspectroscopy.Additional advantagesofthesolid-state13CNMRapproachhasbeenrecentlyreviewedbyDuarte etal. [10],andinclude(1)thedistinctivefeatureofbeinganondestructivetechnique, leavingthesampleavailableforothercomplementarychemicalanalyses;(2)itfacilitatesamuchhighersampleconcentrationthansolution-stateNMR,enhancingsignalsandsavinginstrumenttime;(3)thetechniquedoesnothavesomeofthe problemsreportedforsolution-stateNMRanalysesofNOM,includingsolventeffects onthechemicalshiftsofthesample,potentialmaskingofcertainsamplechemical shiftsduetosolventsignals,andlimitedsolubilityoftheorganicmaterialinthe selectedsolvent;(4)thedetectionofnonprotonatedcarbonsusingsolid-state 13C NMRisstraightforward;and(5)themacromolecularstructuresand/orcolloidswithin NOMslowthetumblingofthesemolecules,leadingto T2 valuesthataretooshortto allowmanyofthepulsesequencesofsolutionNMRtobesuccessfullyused [8,73]. NOMapplicationsofnucleiotherthan 13Chavebeenalsoreportedforsolid-state NMR,includingboth 15Nand 31Pnuclei.AsrecentlyreviewedbyMaoandcoworkers [8], 15NCP-MAShasbeentheprimarysolid-stateNMRtechniqueusedforstudying organicnitrogenformsinNOMfromsoil,water,sediments,coal,andkerogen. However,acquiringameaningful 15NCP-MASNMRspectraofsuchcomplexNOM matricesisratherdifficult.Analternativesolid-stateNMRtechnique, 13C{14N}

saturationpulse-induceddipolarexchangewithrecoupling(SPIDER),hasbeensuccessfullyemployedtoinvestigatethechemicalnatureofnitrogeninNOMbydetecting 13C bondedtonitrogen [8,77,78] 31PsolidsNMRhavebeenreportedformarineDOM [79] andbulksoils [80],beingsuccessfullyusedfortheidentificationofdifferentphosphorus formsandfortheevaluationoftheirdynamicsinthestudiedsamples.

Solid-state2D 1H-13Cheteronuclearcorrelation(HETCOR)NMRispossibleand hasprovedextremelyusefulforassessingthrough-space 1H-13Ccorrelationsand, therefore,acquirevaluableinformationonthestructureofthesurroundingsofcarbon functionalgroups [8,48,75,78].This2Dsolid-stateNMRtechniqueallowstheidentificationofconnectivitiesorproximitiesofdifferentfunctionalgroups(e.g.,aromatic andalkyl),beingparticularlyusefulfortheidentificationofthenearestprotonsfor nonprotonatedcarbons,suchasCOO/NC ]O [75] orquaternarycarbons [48]

ComprehensivemultiphaseandinvivoNMRforanalysis ofnaturalsamples

Comprehensivemultiphase(CMP)NMR,whichintegratesthecapabilitiesofsolutionstate,solid-state,andgel-stateNMRintoasingleapproach,allowstodetectand differentiateallliquids,solutions,andgelsinunalteredsamplesintheirnaturalstate. Gel-phaseNMR,alsoreferredtoashigh-resolutionmagicanglespinning(HR-MAS) NMR,involvesthestudyofsamplesthatare“swellable”and/orinthegelphase [7]. Thesamplesconstituentsareanalyzedafterbeingswolleninapenetratingsolvent (e.g.,DMSO-d6)ortheycanbeanalyzedintheirundriednaturalstatewith wateractingasthenatural“solvent” [7].Forexample,theHR-MAShashugepotential fortheanalysisofsoil,plantmaterials,atmosphericparticles,andsmallorganismsin theirswollensate [59].Insoil,forexample,HR-MASprovidesinformationonthe structuresandassociationsoforganiccomponentsatthesolid-waterinterface [81].Combinedwithsolution-andsolid-stateNMRtechniques,aswellasediting-basedexperimentsasinCMP-NMR,itcanprovideamultidimensionaldetailedinsightintothe organizationofsoilcomponentsandhowthedomainsandassociationschangewith pHandsolvent [12],usingsamplesthatareintheirunalteredstate.Thisapproachhas beenalsoappliedtoexamineoil-contaminatedsoil [82],tostudythemolecularinteractionsandfateduringcontaminantsequestrationinurbansoil [9],aswellasforinvivo2D 1H-13CHSQCidentificationofmetabolitesin 13Cenrichedlivingorganisms [59,83–86], andexaminationofplantsstructureandfunctionintheirnativestate [87]

High-resolutionmassspectrometryinenvironmental research

High-resolutionmassspectrometry(HR-MS)(addressedin Chapter4)isanothersignificantanalyticaladvanceandholdsgreatpromiseinstudiesofcomplexmaterials,such asNOMfromaqueous [1,2,20,61,77,88–90],soils [6,91,92],extraterrestrialorganic matter [19],andorganicmatterinatmosphericaerosols [18,47,93] andrainwater [94] samples.ThemostsignificantadvantageofHR-MStechniquesintheanalysisof

complexmixturesistheirabilitytoprovidehighpeakcapacityandhighmeasurement throughputnecessarytoassignaccuratemolecularweightsand,thus,molecularformulastotheindividualcomponents,withouttheneedforpriorseparation.Asdiscussedby MayandMcLean [44],multidimensionalseparationsbasedonHR-MStechniques exhibitpeakcapacitiesapproaching100,000orgreaterandarecapableofveryhigh peakproductionratesrangingfrom100,000peakspersecondforOrbitrapMS [FouriertransformMS(FTMS)]toover100millionpeakspersecondfortime-of-flight (TOF)MS.Electrosprayionization(ESI)combinedwithFouriertransformioncyclotron resonance(FT-ICR)-MShasbecomeaprevailingmethodtoassignmolecularformulas tothousandsofmoleculesinasinglecomplexorganicmatrix [89].ESIisa“soft”ionizationtechniquethattransfersionsfromsolutiontothegasphasewithminimal fragmentationbeforetheyaresubjectedtoMSanalysis [89].Whiletheapplication ofthisapproachisfairlystraightforwardforwater-solubleNOMfractions,itisof limitedutilityforpoorlysolublematerials,suchassoilorganicmatterunlessone canextractthisorganiccomponentwithlittleornochemicalalteration [6].

AtypicalFT-ICRmassspectrumofcomplexorganicmixtures,suchasthoseof NOM,containsthousandsofindividualpeaks,eachrepresentingauniquemolecular mass,signalmagnitude,andaspecificmolecularformula [89].OncesuchHRmass spectraareobtained,twoimportantissuesneedtobeaddressed:(1)separatenoisefrom analytepeaksinordertoavoidassigningfalsemolecularformulas [90] and(2)find adequatewaystovisualizeandreducetheacquiredcomplexmultidimensionaldata sets [89].IntegratingadditionalseparationdimensionswithFT-ICR-MSprovides additionalcompositionalinformation,butitaddstothecomplexityofanalyzinglarge datasetsproducedbythehyphenatedHR-MSmethod [95].

Inordertoaddressthefirstissue,RiedelandDittmar [90] haverecentlyproposeda newdetectionlimitmethodfortheanalysisofNOMviaFT-ICR-MS,allowingto identifypeaksthatcanreliablybedistinguishedfromnoise.Asexplainedbythe authors,thismethodrequirestheanalysisofreplicateblanks,aprocedureusually implementedtocheckforimpuritiesorcontaminations.Thenoisepeaksfound intheblanksarethenusedtodefinethesignaluncertaintyofthenoise,andpeaks thatareindistinguishablefromthisnoisecanreadilyberemovedfromrealsamples, withsoftwarehelp [90].ThesecondissueinFT-ICR-MSstudiesofcomplexsamples isdatapresentationandexploitation.AspointedoutbyReemtsma [89,96], FT-ICR-MSdatasetsofcomplexorganicmatrices,suchasthoseofNOM,arenot onlylargebutalsomultidimensional,whereforonemoleculethenumberofseveral elementsisknown(C,H,Oasaminimum,butalsoofN,S,and/orP),togetherwithits molecularmass,signalintensity,andretentiontimeincasethatchromatographicseparationisemployed.The2DvanKrevelendiagram(Fig.1.3),whichplotstheH/C ratiosofthemoleculesagainsttherespectiveO/Cratios [89,96,97],isthemost widelyusedgraphicalrepresentationofFTICR-MSdata,producinganillustration ofdifferentcompoundclassesbasedonthemolecularformuladataofthemolecules withinthecomplexmatrix.The2DvanKrevelendiagramcanbefurtherexpandedtoa 3Drepresentation,byaddingionabundanceoranothermolarratio(N/C,S/C)asthe z-axis [97].AsexplainedbyReemtsma [89,96],thevanKrevelendiagramhasitsown disadvantagesbecauseitnormalizestothecarbonnumber,thusdiscardingalargeset ofinformation:differentmoleculesthatexhibitsimilarO/CandH/Cratiosplotatthe

Fig.1.3 SchematicrepresentationoftheVanKrevelendiagramofmajorcompoundclasses identifiedinDOMsamples.

AdaptedfromtheworksofR.L.Sleighter,P.G.Hatcher,Theapplicationofelectrospray ionizationcoupledtoultrahighresolutionmassspectroscopyforthemolecularcharacterisationof NOM,J.MassSpectrom.43(2008)854–64, https://doi.org/10.1002/jms,andA.Nebbioso,A. Piccolo,Molecularcharacterizationofdissolvedorganicmatter(DOM):acriticalreview,Anal. Bioanal.Chem.405(2013)109–24, https://doi.org/10.1007/s00216-012-6363-2.

samepointinthediagram,thuslosinganymass-dependentinformation.Reemtsma [96] suggestedanalternativegraphicalrepresentation,byplottingthenumberof carbonsineachformulavsitsnominalmass(CvsM),wherethemoleculesare classifiedintodifferentcategoriesbasedontheirsumofcarbonandoxygenatoms. However,thisCvsMapproachhasnotbeenemployedasmuchasthevanKrevelen diagramintheFTICR-MSanalysisofcomplexorganicmatrices.

AlthoughFT-ICR-MShasbeenprovedtobehighlysuitableforresolvingthousands ofmolecularformulaswithinacomplexorganicmixture,itsuseincombinationwith othertechniques,forexample,2DNMRspectroscopy(e.g., 1H-1HCOSYandTOCSY and 1H-13CHSQC)offersunsurpassedmolecularresolutionallowinganin-depth descriptionofmolecularskeletonandfunctionalgroupsofthestudiedsamples [19, 20,61,92,98].Forexample,Hertkornetal. [61] usedthismultidimensional FT-ICR-MSand2DNMRapproachtodescribeandcomparethecompositionalfeatures ofDOMinsubtropicalwetlandsfromdifferentregionsaroundtheglobe[Everglades (USA),Pantanal(Brazil),andtheOkavangoDelta(Botswana)],whichareunderthe influenceofdifferentorganicmattersourcesandfloodingevents.Withthisnewmultidimensionalanalyticalwindow,theauthorsconcludedthatwetlandDOMsamples sharevariousmolecularfeatures;however,eachDOMsamplewasuniqueinitscomposition,reflectingspecificenvironmentaldriversand/orspecificbiogeochemicalprocesses [61].Astheneedtogetadeeperinsightintothemoleculardiversityofunknown complexenvironmentalmatricesincreases,thecombineduseofmultidimensional HR-MSandNMRtoolsrepresentsamajorsteptowardanimprovedunderstanding oftheenvironmentalimportanceofsuchcomplexmixtures.

Two-dimensionalcorrelationspectroscopy inenvironmentalresearch

2Dcorrelationspectroscopy(Chapter5)isaversatilechemometrictechniqueintroduced byIsaoNoda(e.g.,Refs. [99–102] referencestherein),whichhasstartedtobecomepopularinenvironmentalresearchinthelast10years.The2Dcorrelationspectroscopyhas beenmostlyusedtoresolveandbetterassignoverlappedpeakstypicallyshowninconventional1DNMRandFouriertransforminfrared(FTIR)spectraofcomplexorganic mixturesfromwater [17,42,103,104],sediments [105],atmosphericparticles [43],and biofilms [106].In2Dcorrelationspectroscopy,thesampleunderspectroscopicstudyis subjectedtoanexternalperturbation(e.g.,temperature,pH,orsalinity),whichinduces systematicvariationsinthespectralsignalintensity.Theobtainedsetofspectra observedasafunctionoftheperturbationvariableisthentransformedintoasetof 2Dcorrelationspectrabyaformofcrosscorrelations,whichdefinestructuralrelationships [99] (anexampleofsuch2Dcorrelationspectraisshown Fig.1.4;inthiscasefor WSOMinatmosphericparticles [43]).Forexample,Abdullaetal. [42,103] appliedthe

Fig.1.4 ExampleofasynchronousmapgeneratedfromCP-MAS 13CNMRspectraof atmosphericaerosolWSOMsamplescollectedduringdifferentseasons,wherethetopandthe rightsidearetheaverage 13CNMRspectra.Redandbluerepresentpositiveandnegative correlations,respectively.

Reprinted(adapted)withpermissionfromR.M.B.O.Duarte,S.M.S.C.Freire,A.C.Duarte, Investigatingthewater-solubleorganicfunctionalityofurbanaerosolsusingtwo-dimensional correlationofsolid-state13CNMRandFTIRspectraldata,Atmos.Environ.116(2015)245–52, https://doi.org/10.1016/j.atmosenv.2015.06.043 (Copyright(2015),withpermissionfromElsevier).

2Dcorrelationtechniqueonasetof 13CNMR, 1HNMR,andFouriertransforminfrared (FTIR)spectraofhighmolecular-weightDOMsamplesisolatedalongasalinitytransect.Bycombininginsightsfromthesespectralprobes,eithercorrelatingthesameor differentspectroscopicprobes(asinhetero-spectral2Dcorrelations)alongthesameperturbation(salinity),theauthorsconcludedthattheDOMsamplesconsistsofthreemajor components[i.e.,heteropolysaccharides(HPS),carboxyl-richalicyclicmolecules (CRAM),andamide/aminosugars]thathavedifferentbiogeochemicalreactivities [42].The2Dcorrelationmapsinvolving 1HNMRspectrafurtherrevealedthemajor compoundclasseswithineachcomponent—forexample,itwassuggestedthatHPS encompassthreemajorcompoundclasses(N-acetylaminosugars,6-deoxysugars, andsulfatedpolysaccharidecompounds),whereasCRAMconsistsofatleasttwocompoundclasses(lignin-likeandcarboxylicfunctionalgroupsofaliphaticnature) [103]

Anotherexampleofcouplingbetween 13CNMRandFTIRprobesthrough2DcorrelationanalysishasbeenusedtogleannewstructuralinformationonWSOMfromfine urbanairparticlescollectedduringdifferentseasons,withthemedianofairtemperature withineachseasonastheperturbationvariablethatpromptstheobservedspectralfeatures [43] (Fig.1.4).ItwasconcludedthattheWSOMsamplesconsistsofatleasttwo classesofcompounds:oneisrichinbothcarboxylicandhydroxylfunctionalgroupsand ithasanaliphaticcharacter,andtheotherentailslignin-derivedstructures [43].

The2DcorrelationanalysishasbeenalsoperformedbetweenFT-ICR-MSand 13C NMRspectraofDOMsamplesfromasalinitytransect [88].Thegenerated2Dcorrelationmapdistributedthemassspectralpeaksbasedontheircorrelationwithspecificcarbonfunctionalgroups(namely,HPSandlignin/CRAM-likecomponents) detectedinthe 13CNMRspectra.AsstatedbyAbdullaetal. [88],thistypeof hetero-spectral2Dcorrelationanalysishasthepotentialtoexpandouranalyticalwindowtowardadeeperunderstandingofcomplexorganicmixturescontainingthousandsofcomponents,thusallowingtogleanin-depthknowledgeonthemolecular structuralfeaturesanddynamicsofsuchcomplexmixtures.Regardlessoftheselected spectroscopicprobe,itisclearthatthestructuralinformationobtainedbymeansof2D correlationanalysiscanbehardlyretrievedbyusingasinglespectroscopic techniquealone.

Fluorescencespectroscopyinthecharacterization ofenvironmentalsamples

Excitation-emissionmatrix(EEM)fluorescencespectroscopyisahighsensitivityand nondestructive3Dtechnique,widelyusedtocompareanddiscernthedynamicsand transformationsofchromophoricdissolvedorwater-extractedorganicmatterin diverseenvironmentalmatrices(freshwater [1,16,107],estuaries [108,109],wetlands [61],soil [110],andatmosphericparticles [13,14,111]).OneadditionalexampleoftheuseofEEMfluorescencespectroscopyforthecharacterizationofDOMin anaquaticecosystemcanbefoundin Chapter6

TheacquisitionofanEEMfluorescencespectruminvolvesthecollectionof sequentialfluorescenceemission(Em)spectraatsuccessivelyincreasingexcitation

(Ex)wavelengths.TheEmspectraobtainedareconcatenatedtoproduceaplotin whichthefluorescenceintensityisdisplayedasafunctionofExandEmwavelengths. ThemainfluorescentgroupsinDOMstudiesthathavebeenidentifiedcorrespondto humic-like,protein-like(tyrosine-andtryptophan-like),andpigment-likesubstances [112,113].EEMfluorescencespectroscopycombinedwithparallelfactoranalysis (PARAFAC)modelinghasmadeitpossibletofurtherresolvethecomplex3D EEMspectraintoitsdominantfluorescentcomponentsandquantifyeachcomponent’scontributiontothetotalfluorescence.Inthisregard,thereaderisencouraged torefertothetutorialofMurphyetal. [114] inthepracticalapplicationofPARAFAC tofluorescencedatasets,usingaDOMfluorescencedataset.Forexample,Singhetal. [109] usedEEM-PARAFACtoexaminethecompositionaldistributionandchromophoricDOMvariabilityinanestuarinesystem.Fourcomponentswereidentifiedby thePARAFACmodel,withthePARAFACsamplescoresbeingusedtoexamine probablelinkagestowetlands,agriculturalsources,andotherwaterbodies.Hertkorn etal. [61] alsousedEEM-PARAFACtodiscriminatechromophoricDOMsamples fromthreesubtropicalwetlands[Everglades(USA),Pantanal(Brazil),andOkavango Delta(Botswana)].Inthiscasestudy,theauthorsreportedanalogiesintheDOMfluorescencepropertiesforthethreewetlandsinsuchawaythatthegeneratedEEMPARAFACmodelwasperfectlyapplicabletothethreewetlands.Whenappliedto investigatethefluorescencefeaturesofchromophoricWSOMinatmosphericaerosols fromdifferentenvironments(urban,forest,marine,andpristine),EEM-PARAFAC aidedintheclassificationandsourceidentificationofchromophoresinatmospheric organicaerosols [13,14,111].TheacquiredEEM-PARAFACdataisofutmost importancetoshedlightonthepivotalroleplayedbytheWSOMintheopticalpropertiesandphotochemicalreactivityofatmosphericorganicaerosols.

AnadditionalinterestingapplicationofEEM-PARAFACanalysiswasshownby Woodsetal. [21],combiningchromatographicseparation(bypolarity)withoffline solution-statemultidimensionalNMRintothecharacterizationofSuwanneeRiver DOMfractions.FindingssuggestedthatboththestructuralfeaturesfromNMRand EEM-PARAFACcomponentsvarywithpolarity [21].Themajorityofthefluorescencesignalsweredominantinthemosthydrophobicfractionswhichwerefound tobeenrichedinstructuresderivedfrombothcyclicandlinearterpenoids [21].The hydrophilicmaterial,ontheotherhand,washighlycorrelatedwithcarbohydrate-type structuresaswellashighcontributionsfromaminoacidfluorescence [21].Thiscombinedapplicationofmultidimensionalanalyticaltechniquessetthebasisfornewanalyticstrategiesaimingatthemolecular-levelidentificationandfurtherunderstanding oftheorigin,structure,fate,andchemicalreactivityofcomplexenvironmental matrices.

Comprehensivetwo-dimensionalchromatography inenvironmentalanalysis

One-dimensionalgasandliquidchromatography(1D-GCand1D-LC,respectively) areundoubtedlysuccessfulanalyticalseparationtoolsinenvironmentalanalysis. When1Dchromatographicseparation,evenafteranoptimizationprocess,stillis

insufficienttoachieveagoodresolutionbetweenco-elutedcompounds,particularly whendealingwithcomplexenvironmentalsamples,itbecomesnecessarytoupgrade theanalyticalprocessbyaddingtwoormoredifferentseparationmechanismsinorder totakefulladvantageofcouplingadvanceddetectionsystems(e.g.,HR-MS).Inthis context,comprehensive2Dgasandliquidchromatography(GC GCandLC LC, respectively)havebecomeattractiveanalyticalapproaches,offeringincreasedpeak capacityandselectivityrelativetoconventional1D-GCand1D-LCseparations, respectively.BothGC GCandLC LCinvolvetheuseoftwoindependent separationmechanisms(i.e.,orthogonal),separatedbyaninterfacecalledmodulator, oftenreferredtoasthe“heart”ofGC GCorLC LC [27,115].Thismodulation interfacehasthefunctionoftransferringfractionsofthefirst-dimension(1D)effluent tothesecond-dimension(2D)column,whilepreservingtheintegrityof 1Dseparation. InbothGC GCandLC LC,thewholesampleissubjectedtomultidimensionaland independentseparationmechanisms,ensuringthattheseparationachievedinany previousdimensionismaintainedinthefollowingone.Inthismethodology,the obtainedchromatogrammustberepresentativeoftheentiresampleand,forthis reason,itisnecessarythatthewholesamplepassesthroughthedetectororatleast inapercentagethatguaranteesitsrepresentativeness [116].Multiplereviewshave discussedthetheoreticalandpracticalaspectsofGC GCandLC LC,including thefundamentalprinciples,instrumentalinnovations,parameteroptimization,and dataprocessingapproaches [26–28,30,37].Inthisregard,interestedreadersshould refertothesereviewworksforadditionalinformationontheaspectsofLC LC and/orGC GCmethoddevelopment.Thissectionsolelyaimstoprovideabrief flavorofthediversityofstudiesusingLC LCandGC GCinenvironmental analysisastheseareaddressedin Chapters7 and 8,respectively.

LC LChasbeenappliedinadiversityofareas,includingbiochemicalanalysis, pharmaceuticalanalysis,analysisofTraditionalChineseMedicines,andpolymer analysis.ReadersinterestedinoneoftheseLC LCapplicationsshouldrefer totherecentreviewworksofStollandCarr [26] andPiroketal. [27].Althoughthere isagreatpotentialtoapplyLC LCinenvironmentalresearch,thisareaisstillin itsearlystages.Thehugecomplexityofenvironmentalmatrices,infact,placesa greatdemandintermsofresolutionpower,challenginganalyststochoosethemost appropriatecolumnswithorthogonalselectivitiesforeachseparationdimension,as wellasaninformation-richdetector.Nonetheless,oneoftheattractivefeaturesfor applyingLC LCintheanalysisofcomplexenvironmentalsamplesisthatitadds additionalinformationonthesesamples(e.g.,polarity,size,andelectrophoretic mobility),whichenhancestheinterpretationoftheirphysicochemicalcomposition, especiallywhenhyphenatedwithMSdetection.Mostenvironmentalstudiesusing LC LCcoupledtohigh-resolutiondetectorshavefocusedeitherontheidentification andquantificationofasmallgroupofpolarcompounds(i.e.,targetedanalysis) [53,117–119] orinthenonselectivesearch(i.e.,untargetedanalysis)andcharacterizationofunknowncomponentsinasample [23–25,51].Bothanalyticalapproaches requireLC LCmethodoptimization(e.g.,couplingofhighlycomplementary(i.e., orthogonal)separationmodes,mobilephasescompositioninbothdimensionsand theircompatibility,flowrates,andtimeofanalysis),aswellasseparationofbackgroundinterferencesfromtheanalytesandaccuracyinthegeneratedLC LCdata.

Givenitsuniversalapplicability,theimportanceofLC LCisexpectedtogrowrapidlyinenvironmentalresearch.Infact,untargetedanalysesusingLC LCcoupledto MSdetectionisapowerfultoolwiththecapabilityofrevealingnewcompositional andyethiddenstructuraldetailsofcomplexenvironmentalsamples,thusavailing newpathwaysofinvestigation—andthisresearchfieldisonlyatitsbeginning.

TheastoundingseparationpowerofferedbyGC GChyphenatedtoeitheruniversalorselectivedetectors,enticestheresearcherstousethisapproachforthetargeted nonpolarcompoundanalysisinenvironmentalmatrices [28,30].UnlikeLC LC, onecanfindintheliteratureahugenumberofenvironmentalstudiesmorefocused onthechemicalinformationprovidedbyGC GCcoupledtoanH-MSdetector ratherthanontheperformanceandoptimizationofthewholemultidimensional analyticaltechnique.Recently,MuscaluandGo ´ recki [28] presentedasystematic reviewofthemostrecentapplicationsofGC GCcoupledwithHR-MSdetectors intheanalysisofpersistentorganicpollutantsinwater,wastewater,leachates,soil, sediments,sludge,andbiota.Thetargetedanalytesincludehydrocarbons,polycyclic aromatichydrocarbonsanditsderivatives,polychlorinatedbiphenylsandpesticides, benzothiazoles,benzotriazolesandbenzosulfonamides,nonylphenolsandtheirderivatives(e.g.,fromproductionofplasticsandsurfactants),steroids,syntheticmusks, personalcareproducts,andpharmaceuticals [28].Complexatmosphericorganic aerosolscontainingvolatileandsemivolatilecompoundshavebeenalsosuccessfully determinedwithGC GC-basedmethods [55].AshighlightedbyMuscaluand Go ´ recki [28],GC GCalsoallowstheseparationofmanyconstituentsofpreviously unresolvedcomplexmixturesofcontaminants.WhenhyphenatedwithaHR-MSor otherMSdetectors,thisGC GCapproachoffersunsurpassedresourcesforthe nonselectivesearchofadiversityoforganicpollutantgroupsthatmightbeenvironmentallyrelevantbutarenotroutinelyanalyzed.Forexample, Chapter8 highlights howGC GCcoupledwithHR-MSdetectionenablesabetterunderstandingof theimpactofenvironmentalexposuresonhumanhealth.Thischapterdiscusses howGC GC-HR-MSmethodsarebeingusedaskeyanalyticalresourcesforthe identificationandquantificationofawiderangeofanalytes(e.g.,persistentorganic pollutants,dibenzo-p-dioxins,andaromaticamines),sometimesfoundonlyintrace amounts,inbodyfluids(e.g.urine,blood,andbreath).

Synchrotron-basedtechniquesasmultidimensional analyticaltools

Theliteratureshowsthattwoimportantsynchrotron(Sr)-basedtechniques—Sr-FTIR andnear-edgeX-rayabsorptionfinestructure(NEXAFS)—canbeusedforelemental speciationaswellasanalysisofthebulkpropertiesandspatialdistributionofcarbon formsinenvironmentalsamples,particularlyinsoils [31,35,120,121].Animportant strengthoftheSr-basedtechniquesisthehighspatialresolutionatthefinescale, whichallowstodrawamultidimensionalmapofthechemicalenvironmentsof organiccarbon,minerals,metals,andmicrobialhabitatsindifferentenvironmental matrices [31,35,36,104,120,122,123].Theabilitytopotentiallydiscernorganic 16

carbonfunctionalgroupsandtheirpixel-scaleassociationswithotherelementsinthe formofmultidimensionalmapsandonscalesofnano-andmicrometerswithinany givensample,maysignificantlyenhancethecurrentunderstandingofthemechanisms responsiblefornutrientandcontaminantmobility,reactivity,bioavailability,andfate intheenvironment [35,120].Thereis,however,adownsideofsuchgrain-scalemultidimensionaldistributionoforganiccarbonandassociatedelements.Accordingto LehmannandSolomon [31],significantconstraintsareencounteredwheninformation onsinglemicro-ornanoscalelocationswithinasampleneedstobescaledtoprocesses observedatthemacroscale(e.g.,insoilorlandscapes).Additionalconcernsthatneed tobeconsideredandfurtheroptimizedwhenusingsynchrotron-basedtechniques includesamplepreparationprotocolsthatpreservethespatialassemblage,control ofradiationdamage,sectioningartifacts,andspectralquantification [31].Amajor obstacletothewidespreaduseofsynchrotron-basedtechniquesinenvironmental studiesisrelatedtothelimitednumberofanalyticalfacilitiesavailableandassociated expertisetoconductsuchresearch [121].Therefore,researchersmustbecautious abouttheenvironmentalproblemstheywanttoaddressbymeansofthesesophisticatedanalyticaltechniques.

Conclusions

Exploringthechemicalcompositionofdifferentenvironmentalmatrices(air,soil, sediments,water,andlivingorganisms)andthebiogeochemicalprocessestaking placeinthosematrices,involvesmanyunknownsandasnearlymanychallenges. Thedifferentmultidimensionaltechniquesintroducedinthischapterandfurther exploredinthisbook,constituteagreatpromiseinenvironmentalresearch.Integratingmultidimensionalseparationandspectroscopicanalysesatmultiplescales,from smallsolublemoleculestomacromolecules,nanoparticlesorevenlargersizedsamplesisusefulfordecodinghighlyheterogeneousenvironmentalmedia(air,soil,sediments,water,livingorganisms,andbodyfluids)withahighdegreeofspecificity.

Notwithstandingthesophisticatedmultidimensionalanalyticaltechniquesthatare beingusedinenvironmentalresearch,twoadditionalmajorchallengesremain:(1) lackofknowledgeandanalyticalexpertisetodealwithsuchadvancedmultidimensionalapproaches,includingprocessingandinterpretationofthevoluminous andcomplexdatasets,and(2)thedevelopmentofexpertiseforsamplingandmonitoringhighlyheterogeneousenvironmentalmatrices(e.g.,airparticles,waters,soils, andsediments)inanextensiveandregularmanner.Withoutimprovementsinthese importantareas,theuseofmultidimensionalanalyticaltechniqueswillnotbenoteworthyinenvironmentalresearch.

Acknowledgments

ThanksareduetoFCT/MCTESforthefinancialsupporttoCESAM(UID/AMB/50017/2019) andprojectAMBIEnCE(PTDC/CTA-AMB/28582/2017),throughnationalfunds(OE).FCT/ MCTESisalsoacknowledgedforanInvestigatorFCTContract(IF/00798/2015).

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