Information Circular--KGS
Archived
This content is available here strictly for research, reference, and/or recordkeeping and as such it may not be fully accessible. If you work or study at University of Kentucky and would like to request an accessible version, please use the SensusAccess Document Converter.
Abstract
Manganese is a common constituent of Kentucky rocks and soils and, along with iron is one of the most widespread causes of problems in groundwater supplies. Rainwater seeping through soils and bedrock dissolves manganese and carries it in the groundwater system to wells and springs. In deep, slow-moving systems that lack oxygen, manganese remains in solution. Under oxidizing conditions, however, such as in shallow groundwater systems or where the water is exposed to air, manganese combines with oxygen to form black particles that can clog plumbing fixtures and stain containers and clothing.
Publication Date
2007
Series
Series XII
Issue Number
Information Circular 14
Digital Object Identifier (DOI)
https://doi.org/10.13023/kgs.ic14.12
Repository Citation
Fisher, R. Stephen and Davidson, Bart, "Groundwater Quality in Kentucky: Manganese" (2007). Information Circular--KGS. 12.
https://uknowledge.uky.edu/kgs_ic/12
