{"refrec":{"BRefID":104396,"RR":"<b>de Looff, D.</b> (1984). De ontwikkeling van de schaaroevers van de overloop van Valkenisse en het Nauw van Bath tot omstreeks 1980. <i>Nota WWKZ</i>, 84.V013. Rijkswaterstaat, Directie waterhuishouding en waterbeweging, district kust en zee, adviesdienst Vlissingen: Vlissingen.  28 + bijlagen pp.","BEntID":98257,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":". <i>Nota WWKZ</i>, 84.V013. Rijkswaterstaat, Directie waterhuishouding en waterbeweging, district kust en zee, adviesdienst Vlissingen: Vlissingen.  28 + bijlagen pp.","DocTypID":13,"DocType":"Reports","MarineFlag":1,"FreshFlag":0,"BrackishFlag":1,"TerrestrialFlag":0,"Authorstring":"de Looff, D.","OrigTitleTranslFlag":0,"Authorstringtrunc":"de Looff, D.","Englishabstract":null,"AbstractOtherLang":"Het bovenstrooms van Hansweert gelegen deel van de Westerschelde wordt reeds sinds omstreeks 1900 door baggerwerken beïnvloed. Sinds 1920 en met name in de periode 1971-1980 was dat in toenemende mate het geval. Naast een toeneming van de hoofdgeulen (doorsneden en volumina) hebben de baggerwerken mede tot een versterking van de inscharing van de schaaroevers langs de Overloop van Valkenisse en het Nauw van Bath geleid. 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