Development
of
a
flow
method
for
the
determination
of
phosphate
in
estuarine
and
freshwaters—Comparison
of
flow
cells
in
spectrophotometric
sequential
injection
analysis
Raquel
B.R.
Mesquita
a,b,
M.
Teresa
S.O.B.
Ferreira
a,
Ildikó
V.
Tóth
c,
Adriano
A.
Bordalo
b,
Ian
D.
McKelvie
d,
António
O.S.S.
Rangel
a,∗aCBQF/EscolaSuperiordeBiotecnologia,UniversidadeCatólicaPortuguesa,R.Dr.AntónioBernardinodeAlmeida,4200-072Porto,Portugal
bLaboratoryofHydrobiology,InstituteofBiomedicalSciencesAbelSalazar(ICBAS)andInstituteofMarineResearch(CIIMAR),
UniversidadedoPorto,Lg.AbelSalazar2,4099-003Porto,Portugal
cREQUIMTE,DepartamentodeQuímica,FaculdadedeFarmácia,UniversidadedePorto,RuaAníbalCunha,164,4050-047Porto,Portugal
dSchoolofChemistry,TheUniversityofMelbourne,Victoria3010,Australia
Keywords:
Sequentialinjection
Phosphatedetermination
Estuarineandriverwater
Spectrophotometry
Multi-reflectiveflowcell
a
b
s
t
r
a
c
t
Asequentialinjectionsystemwithdualanalyticallinewasdevelopedandappliedinthecomparisonof twodifferentdetectionsystemsviz;aconventionalspectrophotometerwithacommercialflowcell,anda multi-reflectiveflowcellcoupledwithaphotometricdetectorunderthesameexperimentalconditions. Thestudywasbasedonthespectrophotometricdeterminationofphosphateusingthe molybdenum-bluechemistry.Thetwoalternativeflowcellswerecomparedintermsoftheirresponsetovariationof samplesalinity,susceptibilitytointerferencesandtorefractiveindexchanges.Thedevelopedmethodwas appliedtothedeterminationofphosphateinnaturalwaters(estuarine,river,wellandgroundwaters). Theachieveddetectionlimit(0.007mMPO43−)isconsistentwiththerequirementofthetargetwater samples,andawidequantificationrange(0.024–9.5mM)wasachievedusingbothdetectionsystems.
1. Introduction
Phosphateisanimportantroutineparameterinwater analy-sis,beingsimultaneouslyanessentialmacronutrientandapossible pollutant,whenitsconcentrationisabnormallyhigh.The quantifi-cationofphosphateindifferentwaterbodiesisimportantsincethe increaseofphosphateconcentrationsinsurfacewatersisusually linkedtodiffusesources(likeagriculturalrun-offs).
Methods applicable tophosphate determinationin adiverse rangeofnaturalwaters(estuarine,river,wellandgroundwaters) withhighlyvaryingintrinsiccharacteristics,areneeded. Addition-ally,effectivemethodsmusthandletheproblemsarisingfromthe salinity gradient,shouldbefast,withlowreagent consumption andshouldprovidethepossibilityofrealtimeassessment.Flow analysistechniquesmeettheserequirements,whichmakethema valuabletoolformonitoringprocesses.
Flowmethods forthedetermination ofphosphate inwaters have been extensively investigated as listed in comprehensive reviewsbyEstelaandCerdà[1],MotomizuandLi[2]and
Mon-∗ Correspondingauthor.Tel.:+351225580064;fax:+351225090351.
E-mailaddress:aorangel@esb.ucp.pt(A.O.S.S.Rangel).
betandMcKelvie[3].Amongthedifferentflowanalysistechniques proposed inthelast twentyyears, sequential injection analysis (SIA)hasgainedparticularattentionforwateranalysis[4].Samples andreagentsaresequentiallyaspiratedtoaholdingcoil,and subse-quentlytransportedtothedetectorbyflowreversal.Theprotocol sequence,responsiblefor thoseactions,is computercontrolled. SIAmethodshave recognisedmeritsof robustnessand versatil-ityenablingthepossibilitytochangethedeterminationconditions withoutphysicalreconfigurationofthemanifolds.Inthisscenario, severalSIA methods have beenreported for the spectrophoto-metric determination of phosphate [5–20]as listed in Table1. However,thesemethodsweregenerallydevelopedforthe appli-cationtoasingletypeofwater(evenwhenothersampleswere alsoused).Withintheseapplications,someweredesignedtocope withthelowconcentrationoftheanalyteandproposeddistinct strategiestohandlethematrixdifferencesandtheinterferents.For seawatersamples,Maetal.[5]adoptedastrategytodirectly con-centratephosphomolybdeniumbluefromthewatersampletoan HLBcartridge,thiswayminimizingsalinityeffectofthesamples, butcompromisedsamplingfrequency.Forwastewaterandmicro algaemedium[11],amixingchamberwasintroducedintoa man-ifoldtoenhancethemixingconditions,andtoachieveadjustable dilutionofthesamplescoupledwiththestandardaddition
pro-Table 1 Sequential injections systems for the determination of phosphate. Detection system Sample P fraction Reagents Dynamic range RSD LOD Determination rate (h − 1) Reference date Spectrophotometric Seawater Soluble reactive phosphorus Molybdate, ascorbic acid 0.034–1.134 m M 2.50% 1.4 nM 6–10 [5] Fluorimetric Coastal waters Phosphate Molybdate, rhodamine (plus ammonia determination) 0.5–5.0 m M – 0.05 m M 100 [6] Fluorimetric Coastal waters Filterable Reactive phosphate (FRP) Molybdate, rhodamine 0.5–5.0 m M – 0.05 m M 270 [7] Fluorimetric River and marine waters Reactive phosphate Molybdate, rhodamine (plus ammonia determination) 0.3–4.0 m M – 0.3 m M 120 [8] Spectrophotometric Urine Phosphate Molybdate, tin(II) chloride 0.01–30 m M 3.90% – 30 [9] Spectrophotometric Beverages, wastewater, urine Orthophosphate Molybdate U p to 20 mg P L − 1 2.4%, 1.8% 100 m g P L − 1 18 [10] Spectrophotometric Water samples Orthophosphate Molybdate, ascorbic acid used in standard addition 62.5–250 ng P (added) 4% 24 m g P L − 1 14 [11] Turbidimetric Urine Phosphate Calcium carbonate inhibition, calcium phosphate crystallisation 0.1–0.8 m g L − 1; 0.2–1.5 g L − 1 0.97–1.90%; 1.1–2.0% 0.01 mg L − 1; 14 m g L − 1 12; 15 [12] Spectrophotometric Water samples Phosphate Molybdate, ascorbic acid 19.9–196.0 m g L − 1 1.22% 9.92 m g L − 1 54 [13] Spectrophotometric Wastewater Phosphate Molybdate, vanadate (plus Si determination) 0.026–0.485 m M 2.10% 7.4 m M 30 [14] Spectrophotometric Waters and sediments Phosphate Molybdate, ascorbic acid 0.2–7 m g L − 1 – 0.1 mg L − 1 75 [15] Spectrophotometric – Orthophosphate Molybdate, ascorbic acid 4–40 m g L − 1 – 4 m g L − 1 48 [16] Spectrophotometric Natural water and effluent stream Phosphate Molybdate, ascorbic acid 0–70 m g L − 1 0.90% 0.5 mg L − 1 18 [17] Spectrophotometric Tap and well waters Phosphate Molybdate, tin(II) chloride (plus Fe(II) determination) 0.1–1 m g P L − 1 4.10% 20 m g P L − 1 7 [18] Spectrophotometric Wastewater Phosphate Molybdate, vanadate U p to 12 mg P L − 1 <1.4% 0.2 mg P L − 1 23 [19] Spectrophotometric Natural and wastewater Orthophosphate Molybdate, vanadate, malachite green, tin(II) chloride U p to 18.0, 0.4, 4.0 mg P L − 1 2.1, 18, 1.7% 0.15, 0.01, 0.01 m g P L − 1 30 [20]
cedure.Foralakeandatapwatersample,WuandR ˚uˇziˇcka[13] appliedthekineticstoppedflowmeasurementmode,whichcan alsocontributetothereduction ofsamplematrix effectsinthe appliedLab-on-ValveSIAmode.Thesamestoppedflowstrategy wasusedearlierbyMas-Torresetal.[14],tosimultaneously mea-surephosphateandsilicateinwastewaters,althoughundercertain conditionsthemutualinterferenceofthetwoanalytescouldbe detected. Another interesting approach presented by the same researchgroup[18]wasbasedontheuseofthesamplesolutionas carriertodetectmultiplicativeinterferencesinthedetermination. Theuseofthesameflowmanifoldandprotocolsequencefor watersamplesofdifferentoriginsdoesnotusuallyleadtogood qualityresults,duetobothchemicalandphysicalinterferences. Forexample,largedifferencesinsamplesalinitymayinduceshifts in theequilibriumofchemical reactions,andalsomayproduce interferencesinthespectrophotometricdetection,bycreatinglight refractioninthereactioninterfaces,seriouslyaffectingthe analyt-icalsignal[21].
Inthiswork,weproposetheuseofamulti-reflectivecell(MRC) [22]coupledtoasequentialinjectionsystemtotacklethis prob-lem.Intheseconditions,theSIAmanifoldprovidesthenecessary “alacarte”in-linesampletreatmentandtheminiaturized spec-trophotometer(MRCwithaLEDlightsourceanddetector)provides detectionwithminimumschliereneffect.Tohighlightthe mer-itsoftheflowcell,amanifoldthatallowsthecomparisonwitha conventionalflowcell(CFC)placedinaUV–Vis spectrophotome-teris presented.TheSIAmethodologywasbasedonthewidely usedphospho-molybdenumbluereaction.Thisreactionhasbeen reportedashighlysensitiveandselectivewithfewpossible inter-ferences,namelyAs(V),SiandGe[23].Thebestconditionsforthe colorimetricreactionwereassessedandtheminimizationof possi-bleinterferenceswaseffectivelycarriedoutin-line.Thedeveloped system, waseffectively appliedto estuarine (salinitygradient), river,wellandgroundwaters.
2. Experimental
2.1. Reagentsandsolutions
Allsolutionswerepreparedwithanalyticalgradechemicalsand deionisedwater(specificconductancelessthan0.1mScm−1).
The 20gL−1 ascorbicacid solutionwas weekly preparedby dissolving2.0gofascorbicacid(Normapur,France)in100mLof deionisedwaterandwaskeptinadarkglassflask.
The molybdate reagent was weekly prepared by dissolving 1.6g of ammonium heptamolybdate-tetra-hydrate fromMerck, Germany(16gL−1), 40mgofpotassiumantimony(III)oxide tar-trate hemi-hydrate fromSigma, Germany (0.4gL−1) and 0.75g of tartaric acid from Merck, Germany (7.5gL−1) in deionised water,followedbyadditionof10mLof6Msulphuricacid from Merck,Germany(0.6M).Afterhomogenisation, deionisedwater wasaddedto100mLandthesolutionwaskeptindarkglassflask. Phosphatestocksolution(29.4mM)waspreparedbydissolving 0.40gofpotassiumdi-hydrogenphosphate(fromMerck,Germany) previously dried in 100mL of deionised water and stored in a refrigerator.Phosphateintermediatestandardsolutionsof595mM and11.9mMwerepreparedeveryfortnightbyappropriate dilu-tionofthestocksolutionandstoredintherefrigerator.Working standards,0.024–9.52mM,werepreparedweeklybyappropriate dilutionandstoredintherefrigeratorwhennotinuse.
2.2. Samplecollectionandpreparation
Differentwatersampleswerecollectedandanalysed:estuarine waters(withasalinitygradientalongtheestuary),riverwaters, wellwatersandgroundwater.
Theestuarinewatersampleswerecollectedfromthreedifferent PortugueseestuarieslocatedinNWPortugal:Ave(41.3◦N,08.7◦W), Cávado(41.5◦N,08.7◦W)andDouro(41.1◦N,08.6◦W)rivers.For
Fig.1.SIAmanifoldforthespectrophotometricdeterminationofphosphate:molybdatereagent,ammoniumheptamolybdate-tetra-hydrate16gL−1,potassiumantimony(III)
oxidetartratehemi-hydrate0.40gL−1,tartaricacid7.5gL−1andsulphuricacid0.60M;ascorbicacid,20gL−1;S,sampleorphosphatestandard;W,waste;PP,peristaltic
pump;HC,holdingcoil,400cmlong;Ri,reactioncoils,270cmlong;SV,eightportselectionvalve;CFC,spectrophotometerat660nmwithaconventionalflowcell;MRC,
eachestuary,thewaterwascollectedfromthesurfaceatthree dif-ferentlocations:atclosetotheocean(location1)andtwoother upstream (locations 2 and 3), location 3 havingthe less influ-encefromtheocean.(MapsoflocationscanbefoundinElectronic SupportingInformation.)
Sampleswerealsocollectedfromthesamerivers,butfurther upstreamfromtherivermouthtoensurethattheywerenot influ-encedbytheestuary,asindicatedbythemeasuredsalinityvalues. Welland ground waterswere alsocollected inthenorth of Portugal.Allthewatersampleswereintroduceddirectlyintothe SIAsystem.Therefore,resultsonphosphateanalysiscorrespondto thefractionofTotalReactivePhosphorous[24].
2.3. Sequentialinjectionmanifoldandprocedure
The sequential injection manifold used for the colorimetric determinationofphosphatewiththetwopossibledetection sys-temsisdepictedinFig.1.
Solutions were propelled by a Gilson Minipuls 3 peristaltic pump,withPVCpumpingtube.Thiswasconnectedtothe cen-tralchannelofaneightportselectionvalve(ValcoVICI51652-E8). AlltubingconnectingthedifferentcomponentswasmadeofPTFE (Omnifit),with0.8mmi.d.
A personal computer (Samsung SD 700) equipped with a PCL818L interfacecard,runninghomemadesoftware writtenin QuickBasic4.5,wasusedtocontroltheselectionvalvepositionand theperistalticpumpdirectionandspeed.
A conventional spectrophotometer (Hitachi UV-Vis, 100-40) wassetatthewavelengthof660nmandequippedwithaHellma 178.711-QS flow-cell (10mm light path, 30mL inner volume). Whiletheoptimaldetectionwavelengthforascorbicacidreduced phosphomolybdateisca.880nm[25],thespectralabsorptionband isverybroad,anda wavelengthof660nmwasselectedforthe spectrophotometerinordertoallowdirectcomparisonwiththe otherdetectionsystemused,whichwasespeciallydesigned multi-reflectiveflowcell(MRC)previouslydescribedbyEllisetal.[22]. ThelightsourceinthisdetectorwasaredLED(maxat660nm)light sourceconnectedtoa12Vpowersupplyregulatedto5Vusinga multimeter.Theoutputvoltagewassetto0VwhiletheLEDwason andusingdeionisedwater.Fordetaileddescriptionofthedetector thereadersshouldrefertotheoriginalpaper[22].Analyticalsignals wererecordedonaKipp&ZonenBDchartrecorder.
Thesequenceofstepswiththerespectivetimeandvolumesfor thedeterminationofphosphateisshowninTable2.
Thefirststepistheaspirationofsample(stepA),followedby theaspirationofthemolybdatereagentandascorbicacid(stepsB andC).Mixingisthenpromotedbythereversaloftheflowwhile propellingtheplugstowardsthedetector(stepH).
Forthelineardynamicrangeof0.025–0.25mM,fourextrasteps (stepsD–G)wereadded.StepsDandEenabletoobtainadouble plugofsampleand reagent,respectively,andthestepsFandG
resultinastoppingperiodbeforethedetermination.Theflowwas stoppedinthereactioncoilfor30stoensurehighersensitivity.
NoadsorptionofmolybdenumblueonthesurfaceoftheTeflon tubingwasobserved,andnocarryoverbetweenpeakswasdetected undertheworkingconditionspresentedinTable2.Yet,theflow systemwasrinsedwithadiluted(0.05M)NaOHsolutionatthe endofaworkingweek.
2.4. Referenceprocedure
Fortheaccuracyassessment,sampleswereanalysedusingthe vanadomolybdophosphoricacidcolorimetricmethod(APHA 4500-PC)[25].Theassayswereperformedintriplicateandquantified fromstandardcurvesprepareddaily.
3. Resultsanddiscussion
3.1. Studyofthedeterminationparameters
Optimizationofthecolorimetricreactionwascarriedoutusing theUV–Visspectrophotometerwiththeconventionalflowcell.The wavelengthwasselectedto660nm,correspondingtothe maxi-mumemissionoftheLEDtobeusedsubsequently.
3.1.1. Aspirationsequencetotheholdingcoil
Accordingto themolybdenumbluechemistry, theintensely colouredcompoundresults fromthereduction ofthe phospho-molybdicacidbyascorbicacid,APHA4500-PE[25].The phospho-molybdicacidresultsfromthereactionbetweenorthophosphate andthemixtureofammoniummolybdate/potassiumantimonyl tartrateinacidicmedium.
Two possible sequences were investigated: sample–molybdenum solution–ascorbic acid and ascorbic acid–molybdenum solution–sample.The results obtained when the sample was aspirated first showed an 8.5% increase in sensitivity,sothisorderwaschosen.
3.1.2. Reagentconcentration
The molybdate reagent solution is composed of ammo-nium heptamolybdate, potassium antimony(III) oxide tartrate and sulphuric acid. Firstly, the sulphuric acid concentration was fixed and the concentration of heptamolybdate and anti-mony(III)oxidetartratewasstudied.Thistestwascarriedoutby maintainingaconcentrationproportionof40:1(ammonium hep-tamolybdatetetra-hydrate:potassiumantimony(III)oxidetartrate hemi-hydrate)asreportedbyMoraisetal.[11].Theconcentration ofammoniumheptamolybdatetetra-hydratewasvariedfrom8to 18gL−1,resultinginaconcentrationrangeof0.20–0.45gL−1 for theantimony(III)compound.Thehighestsensitivitywasobserved for 16gL−1 of ammonium heptamolybdate tetra-hydrate with
Table2
Protocolsequenceforthedeterminationofphosphate.
Step SVposition Time(s) Flowrate(mLmin−1) Pumpdirection Volume(mL) Action
A 1 12/7.5a 3.9 a 780/488a Aspirationofsample/standard
B 2 1.5 2.9 a 72 Aspirationofmolybdatereagent
C 3 3.5 3.9 a 228 Aspirationofascorbicacid
Db 4 1.5 2.9 a 72 Aspirationofmolybdatereagent
Eb 5 7.5 3.9 a 488 Aspirationofsample/standard
Fb 6/7c 17 3.9 b 1105 Propeltoreactioncoil
Gb 6/7c 30 0 – 0 Stopflow
H 6/7c 70 3.9 b 4550 Propeltodetector(l=660nm)andsystemwashing
aTimeandrespectivevolumeforthelineardynamicrange0.025–0.25mM.
bStepsaddedincaseofthedynamicrange0.025–0.25mM.
Table3
Summaryofthechemicalandphysicalparametersstudies.
Parameter Studiedrange Selectedcondition
[(NH4)6Mo7O24.4H2O)](gL−1) 8–18 16 [C4H4KO7Sb](gL−1) 0.20–0.45 0.40 [H2SO4](M) 0.45–0.90 0.45 [C6H8O6](gL−1) 10–50 20 VMolybdatereagent(mL) 51–163 72 Vascorbicacid(mL) 195–325 228 Vsample(mL) 488–910 780
0.40gL−1oftheantimony(III)compoundsothesereagent condi-tionswerechosen.
Theconcentrationofsulphuricacidwasalsostudied;theacidis requiredtoensurethatthepHwas<1inthefinalreactionmixture aswellastoincreasethesolubilityofthereagentcomponents. Con-centrationsof0.45,0.60and0.90Mofsulphuricacidweretested. Withaconcentrationof0.45Mitwasnotpossibletodissolvethe reagents,and aminimumconcentrationof0.60Mwasrequired toobtainfulldissolution.Higheracidconcentrationsresultedina decreaseinsensitivity,so0.60Mofsulphuricacidwasthechosen concentration.
The ascorbicacid concentrationwasalsostudiedwithinthe range 10–50gL−1 and the highest sensitivity wasobtained for 20gL−1,sothatwastheconcentrationchosen.Asummaryofall studiedparametersandthechosenvaluesisshowninTable3. 3.1.3. Lineardynamicrange0.25–9M
Forobtainingthemaximumsensitivityinthisapplicationrange, thestudywasinitiatedbytestingtheinfluenceofthevolumeofthe molybdatereagent(samplevolumesetto488mL,withintherange 1–4mM).Thetestedvolumeswere:51,72,98,and163mL.Avolume of72mLgaveincreasedsensitivityandbetterlinearity,andwasthe chosenvolume.
Optimizationoftheascorbicacidvolumewasperformedwithin therange195–325mL.Thevolumeofascorbicacidwhichprovided thehighestsensitivitywas228mL,sothiswasthevolumechosen. Thisresultcanbeexplainedbythelimitedoverlapping(ormutual dispersion)betweenthereagentandsamplesolutionsinducedby theincreaseoftheascorbicacidvolumeintroducedbetweenthem. Thesamplevolumewasstudiedandavolumeof780mLwas chosenfromtherange488–910mLasitgavethehighestsensitivity. Withthisreassessmentofsamplevolume,alineardynamicrange of0.25–9.5mMwasobtained.
3.1.4. Lineardynamicrangeupto0.25M
Considering that someuncontaminated natural waters may have phosphate concentrations below 0.25mM [26], different approachesweretestedtoachievealowerlimitofquantification. 3.1.4.1. Effectofdifferentreagentsequences—thedoublesampleplug. Toobtainalineardynamicrangeof0.05–0.25mMitisnecessaryto maximizethevolumeofsampleand,atthesametime,to guaran-teeefficientmixingwiththereagents.Toachievebothconditions, thesamplewasintroducedastwoplugs,withoneoneitherside ofthereagent plugs.Aprogram sequenceincludingthedouble plugsforbothsampleandmolybdatereagentwastested.Theorder ofaspirationwiththetwo extraplugswas: sample–molybdate reagent–ascorbic acid–molybdate reagent–sample. The sample volumeofeachplugwassettoabout500mLandthevolumesof molybdatereagentandascorbicacidweremaintainedatthesame valuesderivedfromthepreviousstudy(Section3.1.3).
3.1.4.2. Effect of reaction time—stop-flow. In order to further increasesensitivity,anincreaseinthereactiontimewastested. Aftertheaspirationof alltheplugs,themixturewaspropelled towardsthedetector and thenstopped in thereactioncoil. To ensurethatalltheplugswereinthereactioncoil,thecoillength wassetto270cm,avaluethatwasobtainedfromprevioustests employingadyesolution.Severalstoptimesweretestedranging from0to90sand astoptimeof30swaschosen.While sensi-tivityincreasedwiththeincreasedstoptime,thelinearityofthe calibrationcurvedecreased,soa30sstoptimewasselectedasa compromisebetweensensitivityandlinearityofresponse.
Undertheoptimizedconditionswiththedoublesampleplug setupitwaspossibletoreachthedetectionlimitof0.007mM,and thequantificationlimitof0.023mM.
3.2. Comparisonofthetwopossibledetectionsystems
Theconditionsobtainedfrompreviousstudies(Section3.1)for thelinear dynamicrange of 0.25–9.5mM phosphatewereused (unlessotherwisestated)inordertocomparetherelativemerits ofthetwodetectioncells.
3.2.1. Schliereneffect
Inflowanalysis,thephenomenonknownastheschliereneffect, results fromthedeflectionofthelight beam(signal refraction) causedbythecreatedconcentrationgradient[21]iftherefractive indices of carrier sample and reagents are significantly
differ-Fig.2. SIAtracesshowingacomparisonbetweenthesample(s)andthedeionisedwater(w)peaks:(a)withtheMRC,(b)withtheCFC;andcomparisonofapartialcalibration
ent. Theinterface between thesesolutions canproduce optical lenses andsoa signalresultingoflight deflectionisregistered, schliereneffect.Ifthissignalisconcomitantwiththeonetobe mea-suredatthesamewavelength(lightabsorption),erraticresultsare obtained,withmoreevidenteffectsatlowanalyteconcentrations. This problem is particularly important in SIAsystems because, unlikeFIAmanifolds,noconfluencepointsareusedtoimprovethe mixing.Differentstrategieswereeffectivelyappliedtominimize theimpactofthisphenomenonontheaccuracyandprecisionof spectrophotometricdeterminations,Diasetal.suggestedtheuse of dualwavelength measurement[21] and McKelvieet al.[27] appliedthematrix matchingstrategyforsalinitycompensation. TheMRCwasspeciallydesignedbyEllisetal.[22]tominimize theschliereneffect.ToassessthiscapacityunderSIAbasedflow conditions,sampleandblankwereinjectedandthesignals (ampli-fiedviewinFig.2aandb)werecompared.Theresultspresented onthefigurecorrespondtothedoubleplugprogram(lowerlinear dynamicrange)asthisparticulareffectismorepronouncedwhen increasednumbersofplugsareinjected.SIApeakswereproduced usinganMRCandtheconventionalflowcell,anditcanbeobserved that,whenusingaCFC,thesignalsaremuchmorepronetoerratic signalsclosetothebaseline(Fig.2candd).
TheseresultsindicatethattheSIA-MRCcanbeusedinmatrices withquitedifferentrefraction indices,withnosignificant opti-calinterferenceinthemainsignal.Additionally,theuseofaMRC contributestotheminiaturizationoftheoverallapparatus.This detection system proved to be advantageous for theestuarine watersamples.
3.2.2. Chemicalinterferences
Distinctivelyfromotherspectrophotometricor chemilumino-metricdeterminationsofphosphate,themolybdenumbluemethod isonlysubjecttoasmallvarietyofinterferencesunderflowanalysis conditions.Interferingspeciesinthedeterminationofphosphorous bythephosphomolybdeniumbluemethodareAs(V),SiandGe[23], whichalsoreactwithmolybdatetoformthecorrespondingacids whicharereducedtotherespectiveheteropolybluesbyascorbic acid.
Consideringthattheproposedmethodwasdirectedatnatural waters(estuarine,riverandwellwaters)themostlikely interfer-encewouldbefromsilica.Thisisachemicalinterferencetherefore itwasnotexpectedtoproducedifferentbehaviourinthetwo detec-tionsystem.
Thisinterferencewasassessedatphosphateconcentrationsof 0.25mM,withdifferentamountsofsilicateadded.UsingtheCFC detectionsystem,therewasnosignificantinterferenceuptoa sil-icateconcentrationof32.9mM,howeverwiththeMRCdetection systemsignificant(>5%)interferencewasfoundinthepresenceof 1.3mMsilicate.Theinterference,causedbytheformationof
molyb-dosilicateheteropolyacidcomplexatreducedpHcanexplainthis effect,which becomesmorepronouncedusingthedetectorcell withhighersensitivity.Estuarinewatersareexpectedtobeaffected byseawaterwithvaluesupto60mMofsilica[28].Thepresenceof tartaricacidhasbeenreportedtoeffectivelyreducesilicate inter-ference[23]soitwasaddedtothemolybdatereagent.Different concentrationsoftartaricacidwereused(1.7,3.2,6.4,7.5gL−1)for asilicateconcentrationof65.7mM.Asexpected,withanincrease inthetartaricacidconcentration,therewasadecreaseofthe per-centageofinterference.Thepercentageinterferencedroppedfrom 18%,withnotartaricacid,to2%,withthe7.5gL−1tartaricacid.
So,eventhoughonlysomeestuarinesampleswerelikelytohave silicatevaluesupto60mMofsilica,7.5gL−1oftartaricacidwas includedinthemolybdatereagent.Thereasonforaddingthe tar-taricacidtothemolybdatereagentinsteadoftotheascorbicacid solutionwasbasedontheaspirationorder,toensurethatitcontacts directlywiththesample.
Thepossibleinterferencefromnitratewasalsostudied,atthe concentrationlevelof200mMofnitrate,andresultedin<3% inter-ferenceonthesignalofa 0.25mMphosphatestandard solution. Thisnitrateconcentrationisaboutthemaximumfoundinthese estuarinewaters[29].
3.2.3. Salinityinterference
Astheaimofthedevelopedmethodwastheapplicationtowater sampleswithawidesalinityrange,i.e.:estuarinewaters,astudyof salinityinterferencewasofhighpriority.Thesalinityinterference wasassessedbycomparingcalibrationcurvesusingstandard solu-tionswithdifferentsalinityvalues;thesesolutionswereprepared byaddingsodiumchloridetothestandards.Thesalinityvalues wereadjustedtoanintermediateandamaximumlevelof salin-ityinestuarinewaters,of9‰and19‰,respectively[30],although itisrecognisedthatsalinitiesat35‰canbefoundinestuariesatthe seawardextent,beingalsodependentonthetidalriverflow con-ditions.Thecalibrationcurvewithpurestandardswascompared tothecalibration curvewithstandardswithadjustedsalinities. Theestimatedslopesofthecurveswereassessedattheconfidence intervalsat95%.Thequalityoftheregressionwastestedby resid-ualanalysis(i.e.randomnessandnormality)andbythecoefficient ofdetermination(i.e.R2,whichwasabove0.981inallcases).For theCFCthereisonlyoverlappingofthelimitswhilefortheMRC thereisanalmostperfect overlappingoftheentireinterval. So thesalinityaffectsmorethespectrophotometricdetectionwiththe conventionalcell(Fig.S1inElectronicSupportingInformation). 3.3. FeaturesofthedevelopedSIAmethod
Asummaryofthemainanalyticalfeatures:thedynamic concen-trationrangesforthetypicalcalibrationcurves,limitsofdetection
Table4
FeaturesofthedevelopedSIAmethodwithbothdetectionsystems.
Detectionsystem Lineardynamic
range(mM)
Calibrationcurvea LOD(mM) LOQ(mM) RSD(%)b Determination
rate(h−1) Effluent volume (mL) Spectrophotometer andconventional flowcell 0.30–9.50 A=0.0869 (±0.0035) [PO43−]−0.039 (±0.025); R2=0.999(±0.001) 0.089 0.297 0.6% (2.47±0.02) 0.6% (7.33±0.04) 37 4.6 Multi-reflective flowcell 0.25–7.10 Hc=15.2(±0.5) [PO43−]+2.6 (±1.4);R2=0.998 (±0.001) 0.066 0.219 1.3% (2.92±0.04) 0.2% (7.04±0.01) 37 4.6
aValuesinbracketscorrespondtothestandarddeviation,n=5,oftheequationparameters(interdayprecision).
bValuesinbracketscorrespondtotheconcentrationandthestandarddeviation,n=10(intradayprecision).
(LOD) and quantification (LOQ),repeatability (RSD), determina-tionrateandeffluentproduction,forthetwodetectionsystems, isshowninTable4.
Thetypicalcalibrationcurvescorrespondtoameanoffour cal-ibration curves withthestandard errors betweenbrackets.The LODandLOQofbothlineardynamicrangeswerecalculatedasthe concentrationcorrespondingtothreeandtentimesthestandard deviationoftheblank,respectively,accordingtoIUPAC recommen-dation[31,32].
The repeatabilitywasassessedby calculationofthe relative standarddeviation(RSD)obtainedbythemeanoftenconsecutive injectionsofanestuarinewatersample[31].
Thedeterminationratewascalculatedbasedonthetimespent percycle.Acompleteanalyticalcyclemusttakeintoaccountnot onlythesumoftimesintheprotocolsequencebutalsothetime requiredtochangethevalvepositionandtoactivatethepump.The analyticalcycletook2.6minforthedoubleplugmethod(lower lin-eardynamicrange)and1.6minforthesingleplugmethod(higher lineardynamicrange).
The mostsignificantconclusion that canbedrawnfromthe observations in Table 4is that lower detection and quantifica-tionlimitsareobtainedwiththemulti-reflectivecell.Thismaybe attributedtothehigherblankvalueandanincreaseintheblank variabilityobtainedwhenusingthespectrophotometerequipped withthecommercialflowcell(Fig.2).Thedetectionlimitcanbe furtherdecreasedifneededwiththemulti-reflectivecellandusing thedoublesampleplugstrategypresentedSection3.1.4.
Thereagentconsumptionvaluesforthesingleplugmethod val-ueswere:1.52mgofammoniumheptamolybdate-tetra-hydrate; 28.8mgofpotassiumantimony(III)oxidetartratehemi-hydrate; 0.54mgtartaricacid;4.24mgsulphuricacidand4.56mgascorbic acid.
3.4. Applicationtowatersamples
ThedevelopedSImethodwasusedfortheanalysisofavariety ofnaturalwaters,withdifferentsourcesandcharacteristics,and theresultswerecomparedtotheonesobtainedbythereference procedure.
3.4.1. Phosphatedeterminationinnaturalwaters
Theestuarineandriverwatersampleswerecollectedin differ-entlocationsoftheAveriver,asmentionedinSection2.2.Someof thosesampleswereconsideredestuarinewatersduetotheir prox-imitytotherivermouth;onewasconsideredriverwaterduetothe
distancetothesea.Thereforethesalinityvaluesweresignificantly differentrangingfrom0.4‰to7.2‰.
Somewelland ground waterswere alsoanalysed and their salinityvalueswerenegligibleandwerenotlisted.Thevaluesare reportedin Table5 asmeanwiththestandard deviation(three replicatedeterminationsforeachsample).
TheFtestindicatesthatthevariancedetectedinthereference methodinmostcasesisgreaterthantheonefromtheproposed methods.Therefore, unequal variances wereconsidered[33] in thet-testforthecomparisonofthemeans. Calculated|t|values inTableS1(ESI)forthetwodetectionsystemsindicatethatthe resultsobtainedusingtheMRCbasedSIAsystemshowedabetter overallagreementwiththereferencemethod.
Toevaluateaccuracy,alinearrelationshipbetweentheresults obtained with the reference procedure and each one of the two possibledetection systems,CFC and MRC,was established (Fig.S2intheElectronicSupportingInformation).Theregression of CCFC (mM) vs CRef.Met. (mM) resulted in the linearequation: CCFC=0.930(±0.196)×CRef.Met.−0.004(±1.199),R=0.953.The lin-earrelationshipbetweenCMRC(mM)andCRef.Met.(mM)resulted intheequation:CMRC=0.966(±0.133)×CRef.Met.+0.185(±0.811), R=0.979.Thevaluesinparenthesisrepresentthe95%confidence limits.Inbothcasesthefiguresshowthattheestimatedslopeand interceptdonotdifferstatisticallyfromvalues1and0,respectively. Therefore,noevidenceofsystematicdifferencescanbepointedout betweenthetwosetsofresults[33].
3.4.2. Recoverystudiesforseveraldifferenttypesofwater samples
Tofurtherassesstheefficacyofthedevelopedsystem, recov-erystudieswereperformedonwatersamplespreviouslycollected fromotherestuariesinthenorthofPortugal(Section2.2)andstored frozen.
Sampleswerespikedwithvolumesof100mL,120mL,150mL and160mLofphosphatestandardsolution(595mM)wereadded to10or20mLofsample.Thecalculationoftherecovery percent-agewasmadeaccordingtoIUPAC[34].Theanalysiswascarried outusingbothdetectionsystems(TableS1inElectronic Support-ingInformation).
TheSIAmethodologyprovidedrecoveryratioswithanaverage of98%(standarddeviation6.1%)and100%(standarddeviation5.5%) fortheCFCandMRC,respectively.Astatisticaltest(t-test)showed thatfora95%significanceleveltherecoveryvaluesdidnotdiffer from100%asthecalculatedt-valueswere1.639and0.096with correspondentcriticalvalues2.475and2.445fortheCFCandMRC,
Table5
Applicationofthedevelopedsequentialinjectionmethodwiththetwopossibledetections,theconventionalflowcellwiththespectrophotometer(SIA-CFC)andthe
multi-reflectivecell(SIA-MRC)tothephosphatedeterminationindifferentwatersamplesandcomparisonwiththereferenceprocedure(Ref.Met.);SD,standarddeviationfrom
3replicas,RDrelativedeviation.
Sampletype SampleID Salinity(‰) Ref.Met. SIA-CFC SIA-MRC
[PO43−]±SD(mM) [PO43−]±SD(mM) RD(%) [PO43−]±SD(mM) RD(%)
Estuarinewater(Averiver) A1 5.9 6.94±0.14 5.93±0.05 −14.6 6.72±0.02 −3.2
A2 1.2 6.13±0.28 5.87±0.03 −4.2 6.16±0.01 0.5 A3 0.1 6.53±0.01 6.34±0.05 −2.9 6.35±0.01 −2.8 A4 7.2 4.75±0.14 3.82±0.02 −19.5 4.71±0.03 −0.7 A5 0.8 5.89±0.14 5.60±0.03 −4.9 5.86±0.02 −0.5 A6 0.1 6.54±0.24 6.31±0.05 −3.5 6.32±0.01 −3.3 A7 6.5 7.84±0.14 7.40±0.05 −5.6 8.05±0.01 2.7 A8 1.1 5.40±0.14 5.59±0.01 3.5 5.75±0.02 6.6 A9 0.5 6.94±0.14 6.82±0.04 −1.8 7.40±0.01 6.6 Groundwater G1 – 3.53±0.01 3.36±0.06 −4.8 3.54±0.03 0.3 G2 – 8.41±0.14 7.30±0.03 −13.2 7.88±0.01 −6.2 Wellwater W0 – 4.23±0.15 4.35±0.04 2.9 4.58±0.01 8.3 Riverwater R0 0.4 4.10±0.01 3.05±0.02 −25.6 3.68±0.01 −10.3
respectively,thusindicatingtheabsenceofmultiplicativematrix interference[33].
4. Conclusions
Thedevelopedmethodenabledtheevaluationoftwo alterna-tivedetectioncellsunderthesameexperimentalconditions,and resultedinaSIAprocedureforphosphatedeterminationapplicable todifferenttypesofwaterwithhighsalinityandlargematrix vari-ability.Theuseofasequentialinjectiontechnique,tofullyexplore itsversatility,provedtobeasuitablechoice.Theapproachofusing twoprotocolsequences,resultingintwolineardynamicranges, canbeappliedtosampleswithtraceconcentrationoftheanalyte. Incomparing thetwodetectionsystems,themulti-reflective flowcellprovedtobebetterforlowerphosphateconcentrations withanachievabledetectionlimitof0.007mM.
Withrespecttothepossibleinterferencesofsilicate,the inter-ference was effectively minimized, in-line, by adding tartaric acid to themolybdenum reagent. The percentage interference, observed for 68mM of silicate, decreased from18% to 2% asa result.
Whencomparedtopreviouslydescribedproceduresbasedon thesameprinciples(Table1),themostsignificantadvantageofthe workdescribedistheuseofasinglemanifoldforthedetermination ofphosphateindifferentmatrices(well,estuarine,river,andsea waters).Theachievabledetectionlimitcomparesfavourablytothe previouslypublishedSIalternatives(Table1)withouttheneedfor apre-concentrationprocedure.Theanalysedwatersampleswere comparedtoareferenceprocedureandprovedtheaccuracyofthe developedmethodforbothdetectionsystems.
Acknowledgements
R.B.R.MesquitathankstoFSEandFundac¸ãoparaaCiênciae aTecnologia(FCT,Portugal)thegrantSFRH/BPD/41859/2007.I.V. Tóth thanksFSEand MinistériodaCiência, TecnologiaeEnsino Superior(MCTES)forthefinancialsupportthroughthePOPH-QREN program.TheauthorsthankFCTfinancialsupportthroughproject PTDC/AMB/64441/2006,andPeterEllis,MonashUniversity,forthe kindprovisionofthemulti-reflectionflowcell.
AppendixA. Supplementarydata
Supplementarydataassociatedwiththisarticlecanbefound,in theonlineversion,atdoi:10.1016/j.aca.2011.06.002.
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