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Origin of the groundwater salinization in La Aldea coastal aquifer (Gran Canaria, Canary Islands)

Abstract

Groundwater chemistry in La Aldea aquifer (Gran Canaria, Canary Islands) shows high contents of chloride and nitrate ions. The salinization process has been modelled using the geochemical data, taking into account the results of a previous flow model. The results allow to identify the salinity of the recharge from the rainfall under aridity conditions and the irrigation returns like the main causes of the groundwater salinization.

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Origin of the groundwater salinization in La Aldea coastal aquifer (Gran Canaria, Canary Islands)

Author: Cruz-Fuentes, Tatiana,Cabrera, M.C.,Heredia-Díaz, Javier
Year: 2010
Source: https://accedacris.ulpgc.es/jspui/bitstream/10553/9186/4/0673532_00000_0000-1.pdf
P oceedings
J,ne21-2612010
SWI M21
Azo es·
Po ugal
21s
Sa~
Wa e
In usion
Mee ing
O igino  heg oundwa e saliniza ioninLaAldeacoas alaqui e 
(G anCana ia,Cana yIslands)
T.C uz1,M.C.Cab e a1andJ.He edia2

1[email p o ec ed]&mca[email p o ec ed]
Depa men o Physics,Uni e si yo LasPalmasdeG anCana ia,35017
LasPalmasdeG anCana ia(Spain)
2[email p o ec ed]
GeologicalSu eyo Spain,RíosRosas,23.28003Mad id(Spain)
ABSTRACT
G oundwa e chemis yinLaAldeaaqui e (G anCana ia,Cana yIslands)showshigh
con en so chlo ideandni a eions.Thesaliniza ionp ocesshasbeenmodelledusing
hegeochemicalda a, akingin oaccoun  he esul so ap e ious lowmodel.The
esul sallow oiden i y hesalini yo  he echa ge om he ain allunde a idi y
condi ionsand hei iga ion e u nslike hemaincauseso  heg oundwa e 
saliniza ion.
INTRODUCTION
LaAldea a ine,loca edon hewes e nsideo G anCana ia(Cana yIslands,Spain),p esen sa
la bo omsu oundedbyhighmoun ains(wi hheigh s a ying omseale el o1,415m).The
clima eisd ysub opicalwi hhigh empe a u es h oughou  heyea .In ensi eg eenhouse
ho icul u e(mainly oma oesandcucumbe s)isp ac icedwi hacul i a ionsu aceo 645ha
andi iga ionwa e ismainlysuppliedby h eedamssi ua edups eam,al houghmo e han
370la ge‐diame e wellsalsop o idec opwa e  equi emen sin hed yseasons,diminishing
hequali yo g oundwa e .

Thegeologyo  hea eashowsasedimen a yuni ,he e ogeneous,composedo allu ialand
sc eesdeposi s(consis ingo de i icalma e ialwi hphonoli es‐ achy es,ignimb i esand
basal sboulde s)anda olcanicuni ,alsohe e ogeneous,consis ingo Miocenebasal sloca ed
benea h hesedimen a yuni andoccupies heen i esu acewi halowe pe meabili y han
heallu ialdeposi s(Figu e1).The eisa esidual elie loca edeas o  hes udya eabe ween
Fu elandLaAldea a ines(LasTabladas)wi hacomplexgeology,whe eslidhyd o he mal
deposi s(Azulejos)c opsou .

G oundwa e  lowsmainly h oughallu ialma e ials omeas  owes along heLaaldea
allu ial, ha  ep esen sadischa gea ea om heaqui e  o hesea.The eisalsoanimpo an 
low ommoun ainousa easloca edno handsou h owa ds heLaAldeaallu ial.Wa e 
balancehasbeendone o  hehyd ologicalyea s1991‐1999(C uz,2008)andshows ha  he
echa geisa esul o i iga ion e u ns(60%)and ain all(20%).

Thehyd ogeochemis yo  hea eahasbeens udiedsince1992du ingse e al esea chp ojec s
ino de  oquali a i elycha ac e izeLaAldeaaqui e (Muñoze al.,1996;Muñoz,2005;C uz;
2008).Thehyd ogeochemicalconcep ualmodelwases ablishedandsugges s ha awa e  low
ombasal s o heallu ialexis s,and he e o e heex ac edwa e  ep esen amixingo wa e 
ombo huni s.
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G oundwa e in hea eap esen shighsalini y a ios(Clcon en sup o7000mg∙L‐1andN
con en sup o700mg∙L‐1)insomeplaces,and heo igino salini yis heaimo  hep esen 
communica ion.



Figu e1.Localiza iono LaAldeaaqui e inG anCana ia(Cana yIsland,Spain)andgeologicmap
showing hemaingeologicaluni s.

METHODS
In hiswo k, hespa ialand empo aldis ibu iono chlo ideandni a eionsandchemical
cha ac e is icso  hedi e en sou ceso  echa geha ebeens udied oquan i y hein luence
o  hedi e en sou ceso salini y(mainlysalini yo  ain alldue oa idi yandi iga ion
e u ns).Theaqui e salini yhasbeenmodeledalonga lowline(wi h h ee ep esen a i e
wells)in heaqui e (Figu e1)usingPHREEQC.Themodelhassimula edmixingp ocesses
be ween echa gewa e ( ainandi iga ion e u ns)andg oundwa e andchemical eac ions
ha occu insoiland ocksindi e en a easo  heaqui e .

RESULTS
Figu e2shows hespa ialand empo ale olu iono chlo ide o  heyea s1992and1999.The
highes concen a ionsa eobse edinLasTabladas oo and esul s om heleachingo  he
Azulejos.Thelowe concen a ionswe e oundin heMiocenebasal sin hehighes le els.In
gene al, he eiscoincidencebe ween hedi ec iono g oundwa e  lowand heinc easein
chlo ideconcen a ion.Compa ingbo hyea s,aninc easeinchlo ideconcen a ionsis
obse ed.Thea e ageconcen a iono chlo idein hes udya eais711mg∙L‐1 o 1992and
1110mg∙L‐1 o 1999.

Thea e ageconcen a iono ni a esis88mg∙L‐1 o 1992and175mg∙L‐1 o 1999which
ep esen sasubs an ialinc easein heconcen a ion o  his imepe iod, eachingmaximum
alueso 484mg∙L‐1 o 1992and708mg∙L‐11999.Figu e2shows hespa ialand empo al
e olu iono ni a eionshowing ha maximum aluesa eloca eda  hemou ho  he
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Tocodomán a ineand hesou he no LaAldea a inein1992andin1999high alueso 
ni a esoccupymos o  heallu ialloca ed ha iswhe emos c opsa eloca ed.




Figu e2.Isoconcen a iono chlo ideandni a e o 1992and1999.

DISCUSSIONANDCONCLUSIONS
Di e en hyd ogeochemicalp ocesses ha con olg oundwa e geochemis yha ebeen
iden i iedandquan i ied.Rainwa e  ep esen s he20%o  echa ge ha joins heaqui e wi h
ex asaliniza iondue osalini yo  he echa ge om he ain allunde a idi ycondi ions
(Cus odio,1993).I iga ion e u ns ep esen s60%o  he echa geandcausesinc easedsalini y
due o hehighe apo anspi a ion a es.Finally,o he geologicalinpu o highsalini ywa e sis
loca eda LasTabladashasbeena ibu ed oleachingo  hedeposi sknownasAzulejos.

Chlo ideconcen a ionin ainwa e  anges om30mg∙L‐1and450mg∙L‐1ina eas a he and
nea e  hesea espec i ely(Munoz,2005;Alcala,2005,C uz2008).Rainwa e e apo a ionhas
beencalcula edbe ween60%and70%(C uz,2008)p oducinganinc easein hesalini yo  he
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echa ge.I iga ion e u nswa e sha eani a econcen a iono mo e han650mg∙L‐1(C uz,
2008)TheAzulejosin luencehasbeens udied om hechemis yo someoozesloca edinLas
Tabladaswi hwa e s ha ha echlo ideconcen a ionso mo e han8000mg∙L‐1andni a e
concen a ionabo e500mg∙L‐1.

Themodelinghasbeenca iedou  ep oducing hechlo ideandni a econcen a ionin wo
wellsloca edin hemiddleandlowpa o LaAldea a ine(0779‐TPand0218‐O1, espec i ely)
om hewellwa e 2714‐TPloca eda heade (Figu e1)assuming ha allni a ecomes om
i iga ion e u nsandchlo ide echa geby ain all.Thes udyo  hechemicale olu iono 
g oundwa e in he lowline(2714‐TP o0779‐TPand2714‐TP o0218‐O1)shows ha  hewell
0779‐TPp esen s2%o ma inewa e  espec  o2714‐TPand hewell0218‐O1p esen s4%o 
ma inein luence espec  o2714‐TP.Thismeansama inecon ibu iono 0.5%pe kmin he
lowline o 0779‐TP, anging o0.7% o 0218‐O1.Thisinc easein he a eo ma inesp ay
con ibu iono 0.2%in0218‐TPsha wi h espec  o hewell0779‐TPimpliesaninc easein he
con ibu ionasweapp oached hecoas ,whichalsocon i m ain allchemicalda a.

A ending o hemodel esul s, heg oundwa e  ecei es51%o i iga ion e u nsin hewell
0779‐TPand89%in hewell0218‐O1.Thisdemons a es heimpo anceo i iga ion e u ns
wa e asinpu  o hesys emandasasou ceo con amina iono g oundwa e andcon i ms
ha g oundwa e p esen smo ein luenceo i iga ion e u nsasmo ingin hedi ec iono 
low.

REFERENCES
Alcalá,F.J.2005.Reca gadelosacuí e osespañolesmedian ebalancehid ogeoquímico.Doc o al
Thesis.TechnicalUni e si yo Ca alonia.
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C uzT.,2008.Con ibucióndelamodelaciónnumé icaehid oquímicaalconocimien odelacuí e o
deLaAldea(G anCana ia,IslasCana ias).Doc o alThesisUni e si yo LasPalmasdeG an
Cana ia.
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Cus odio,E.,1993.Coas alaqui e saliniza ionasaconsequenceo a idi y: hecaseo Amu ga
phonoli icmassi ,G anCana iaIsland.InE.Cus odioandA.Galo é(eds.):S udyand
modelingo sal wa e in usionin oAqui e s.Ed.CIHS/CIMNE,Ba celona,81‐98.
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Muñoz,J.,2005.Funcionamien ohid ogeológicodelAcuí e odeLaAldea(G anCana ia).Doc o al
ThesisUni e si yo LasPalmasdeG anCana ia.
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Muñoz,R.,Cab e a,M.C.,He nández,F.andSoco o,A.R.1996.De elopmen o Analy icaland
SamplingMe hods o P io i yPes icidesandRele an T ans o ma ionP oduc sinAqui e s.
FinalP ojec Repo .


Con ac In o ma ion:Ta ianaC uz,Uni e si yo LasPalmasdeG anCana ia.Depa men o 
Physics,Uni e si yo LasPalmasdeG anCana ia,35017LasPalmasdeG anCana ia(Spain),Phone:
+34928458080,Fax:+34928452922,Email:[email p o ec ed]

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