Assertion: aquifer's water | /r/AtLocation | contact
Facets:
value: for a long time
type: TEMPORAL
value: with these materials
type: OTHER
value: with aquifer minerals
type: OTHER
value: generally
type: DEGREE
value: with limestone
type: OTHER
Source sentences:
text: The "bad water line" is a natural phenomenon that occurs along the southern and eastern edges of the fresh water zone where water has been in contact with limestone for a long time.
text: Water from the Springfield Plateau aquifer typically has the lowest levels of mineralization, and is a calcium-bicarbonate type of water, reflective of the limestone that the water has been in contact with.
text: The chemical quality of natural ground water is primarily affected by the mineralogy of aquifer materials and the length of time that the water is in contact with these materials; for example, a plot of the relation of boron and sodium to rock types in Michigan (fig.
text: Water deep within an aquifer, as well as that near the end of a long flow path, has generally been in contact with aquifer materials for a long time, which results in large concentrations of dissolved constituents.
text: The lower Cretaceous aquifers contain water with dissolved-solids concentrations of greater than 3,000 milligrams per liter in most of North Dakota, because the water has moved along flow paths hundreds of miles long, has been in contact with aquifer minerals for a long time, and has partially dissolved the mineral material.