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The Clogging of Shallow Discharge Wells in the Netherlands River Region
Author(s) -
Beek C.G.E.M.,
Kooper W. F.
Publication year - 1980
Publication title -
groundwater
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.84
H-Index - 94
eISSN - 1745-6584
pISSN - 0017-467X
DOI - 10.1111/j.1745-6584.1980.tb03652.x
Subject(s) - clogging , silt , chlorine , aquifer , carbonate , calcium carbonate , sodium carbonate , environmental engineering , geology , lime , environmental science , mineralogy , groundwater , chemistry , sodium , metallurgy , materials science , geotechnical engineering , geomorphology , geography , paleontology , archaeology , organic chemistry
A serious type of clogging occurs in wells which abstract anaerobic water from the shallow aquifer in the river region in The Netherlands. These clogged wells can easily be regenerated by means of sodium hypochlorite (15%). The figure for the specific yield after regeneration approximates to the figure on commissioning. During the pumping to waste to clear the well after regeneration, the types of reaction products present in the spent chlorine solution were investigated. From this it can be deduced that the chlorine solution added was utilised mostly for the oxidation of iron sulphides. The remainder was used mainly for the oxidation of organic material. At the same time, calcium carbonate went into solution and iron carbonate was formed. During the regeneration of a number of wells, some silt was also removed. Although information can be obtained in this way about the composition of the materials removed, it is impossible to form any concept of the nature in which these substances are present around the clogged wells.