A Natural Resource Management Guide for the County of Morris A ...
A Natural Resource Management Guide for the County of Morris A ...
A Natural Resource Management Guide for the County of Morris A ...
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Results <strong>of</strong> <strong>the</strong> investigation, based on modeled projections <strong>for</strong> increased pumpage, indicated:<br />
decreased discharge to <strong>the</strong> river from <strong>the</strong> aquifer system;<br />
!<br />
increased downward flow from and decreased upward flow to lower valley-fill aquifer;<br />
!<br />
increased lateral flow <strong>of</strong> ground water into S. Branch Raritan River basin from Lamington River Basin;<br />
!<br />
and slight increase in tributary-stream leakage to aquifer system. 7<br />
!<br />
A connection between human activities and ground water quality was validated by volatile organic compounds<br />
found in each water bearing unit, in addition to concentrations <strong>of</strong> nitrates and chloride.<br />
Ground Water Quality In <strong>Morris</strong> <strong>County</strong><br />
Ground water quality data <strong>for</strong> <strong>the</strong> county is piecemeal. Ground water quality in <strong>the</strong> Highlands is very good<br />
<strong>for</strong> most purposes, with some local areas requiring treatment <strong>for</strong> undesirable characteristics and constituents.<br />
Occasionally State-recommended secondary drinking water standards (those affecting aes<strong>the</strong>tics, e.g.,<br />
appearance, taste, or odor) were exceeded. These parameters included corrosivity, hardness, iron, manganese,<br />
8<br />
sodium and gross alpha particle activity. Primary drinking water standards pertain to potential <strong>for</strong> adverse<br />
affect on human health.<br />
During <strong>the</strong> early eighties' investigation <strong>of</strong> <strong>the</strong> Pequannock River and upper Rockaway River watersheds,<br />
chemical analyses <strong>of</strong> <strong>the</strong> ground water resulted in good to excellent quality designations. Total Iron and<br />
Manganese were <strong>the</strong> only parameters in excess <strong>of</strong> potable water standards. Specific examples <strong>of</strong> this occurred<br />
in samples from some municipal wells in Mountain Lakes and <strong>the</strong> Town <strong>of</strong> Boonton. These wells, adjacent<br />
to <strong>the</strong> Rockaway River and tapping <strong>the</strong> stratified drift aquifer, were receiving Iron and Manganese loads from<br />
infiltrating surface water. Though excessive levels <strong>of</strong> Iron and Manganese pose an aes<strong>the</strong>tic problem, as in<br />
staining <strong>of</strong> sinks and fabrics, <strong>the</strong>y are not considered a health problem.<br />
9<br />
The Passaic River Coalition's investigation <strong>of</strong> <strong>the</strong> Buried Valley aquifer system revealed limited incidences<br />
<strong>of</strong> high sulfate levels. These were associated with sulfate minerals occurring in basalt and red shale. The sand<br />
and gravel aquifers also exhibited increased incidences <strong>of</strong> hard water.<br />
<strong>Management</strong> Considerations<br />
Variables including human health, status <strong>of</strong> ecological resources, cost <strong>of</strong> water treatment and provision <strong>of</strong><br />
alternative supplies justify comprehensive groundwater management. Since activities on <strong>the</strong> land impact <strong>the</strong><br />
quality and quantity <strong>of</strong> ground water and its recharge areas, emphasis is on land use management. With<br />
drawdown occurring in <strong>the</strong> sou<strong>the</strong>ast, regular water shortages in <strong>the</strong> northwest, contamination to <strong>the</strong> east and<br />
elsewhere, <strong>the</strong>re is an obvious need <strong>for</strong> greater geotechnical research on <strong>the</strong> extent and capability <strong>of</strong> bedrock<br />
as well as surficial aquifers.<br />
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64<br />
Ground Water