{"refrec":{"BRefID":118754,"RR":"<b>Baetens, J.; Scheltjens, T.; Van Eerdenbrugh, K.; Peeters, P.; Danckaerts, C.; Maeghe, K.; Meire, P.; Mostaert, F.</b> (2006). Omgaan met watertekorten in het Albertkanaal en de Kempense kanalen. <i>Water: Tijdschrift over Integraal Waterbeleid 25</i>: 48-54","BEntID":113001,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>Water: Tijdschrift over Integraal Waterbeleid 25</i>: 48-54","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Baetens, J.; Scheltjens, T.; Van Eerdenbrugh, K.; Peeters, P.; Danckaerts, C.; Maeghe, K.; Meire, P.; Mostaert, F.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Baetens, J. <i>et al.</i>","Englishabstract":null,"AbstractOtherLang":"Het water dat door het kanalenstelsel van het Albertkanaal en de Kempense kanalen stroomt, is afkomstigvan de Maas. Het Maaswater wordt aangewend voor het verschutten van schepen, de koeling vanelektriciteitscentrales en industriële productieprocessen, drinkwaterproductie, als proceswater voor industrie,bevloeiing van landbouw- en natuurgebieden e.a. en dit zowel in Vlaanderen als in Nederland. Debeschikbaarheid van dit water wordt daarbij vaak als vanzelfsprekendheid beschouwd aangezien er zich totop heden geen noemenswaardige problemen hebben voorgedaan. Een extreme droogteperiode zoals deze van1976 zorgt nochtans voor een aanzienlijke vermindering van de Maasafvoer. Sinds 1976 is het gebruik vanhet Maaswater aanzienlijk toegenomen. Om de gevolgen van een droge periode door deze toename in teschatten, werd een computermodel opgemaakt van het kanalenstelsel waarmee het watergebruik van 2002werd gesimuleerd bij een wateraanvoer van de Maas anno 1976 en 2003. 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