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Ammonium Ion, Humic Materials, and Trihalomethane Potential in Northeastern Kansas Ground Waters
Author(s) -
Denne Jane E.,
Hathaway Lawrence R.,
McCool S. Patrick
Publication year - 1984
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.1745-6584.1984.tb01444.x
Subject(s) - environmental chemistry , nitrate , groundwater , dissolved organic carbon , ammonium , maximum contaminant level , bedrock , aquifer , trihalomethane , total organic carbon , water quality , environmental science , pennsylvanian , surface water , hydrology (agriculture) , chemistry , geology , environmental engineering , water treatment , ecology , geomorphology , geotechnical engineering , organic chemistry , structural basin , biology
Glacial buried‐valley aquifers serve as primary sources of potable ground water in northeastern Kansas. A long known problem, however, is that a large percentage of well waters in this region exceed the U.S. Environmental Protection Agency (EPA) limits for nitrate (NO − 3 ). A detailed study of the hydrogeology and water quality of the buried valleys has confirmed the nitrate problem and led to a recognition that some well waters with low ( 5 mg/l) NO − 3 concentrations have anomalous ( 0.5 mg/l) ammonium ion (NH + 4 ) levels, with an NH + 4 range from <0.1 to 4.8 mg/l. The extractable NH + 4 concentrations in related glacial sediments range up to approximately 75 mg/kg, and the amounts generally increase from an average of 2 mg/kg in the topsoil downward to bedrock. Migration of brines from subjacent Permian or Pennsylvanian bedrock into the unconsolidated sediments locally may cause desorption of NH + 4 and an increase in its levels in the associated ground waters. Numerous test holes drilled in the study area showed a black scum on the fluid and cuttings, which may be from buried humic materials. Recently measured total organic carbon (TOC) contents of the ground waters confirm a significant level in some areas, with a range from 0.1 to 2.4 mg/l as C. Chlorination of water with dissolved organics may lead to production of halogenated compounds. Two public‐water‐supply well waters contained total trihalomethane (TTHM) levels close to the maximum contaminant level (MCL) of 100 /μg/l in chlorinated samples quenched after one week. The presence of NH + 4 inhibits the formation of THMs, but it also can give rise to odor and taste problems in the finished water. The inhibition of THM formation by NH + 4 is achieved by reactions which compete with the organics for combination with chlorine. These reactions make maintaining appropriate chlorine residuals difficult and also may lead to production of undesirable side products. Present efforts to evaluate the regional water‐quality problems are focused in Nemaha County, Kansas.