Author : Daniel R. Norton
Publisher :
Page : 52 pages
File Size : 31,9 MB
Release : 1991
Category : Chlorides
ISBN :
[PDF] Chloride Flux And Surface Water Discharge Of Yellowstone National Park 1982 1989 eBook
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Chloride Flux and Surface Water Discharge Out of Yellowstone National Park, 1982-1989
Author :
Publisher :
Page : pages
File Size : 29,66 MB
Release : 1991
Category :
ISBN :
Chloride Flux and Surface Water Discharge of Yellowstone National Park, 1982-1989
Author : Daniel R. Norton
Publisher :
Page : 42 pages
File Size : 48,98 MB
Release : 1991
Category : Chlorides
ISBN :
Chloride Flux and Surface Water Discharge Out of Yellowstone National Park, 1982-1989
Author : Daniel R. Norton
Publisher :
Page : 25 pages
File Size : 16,27 MB
Release : 1990
Category : Chlorides
ISBN :
Chloride Flux and Surface Water Discharge Out of Yellowstone National Park, 1982-1989
Author : Daniel R. Norton
Publisher :
Page : 42 pages
File Size : 42,83 MB
Release : 1991
Category : Chlorides
ISBN :
U.S. Geological Survey Bulletin
Author :
Publisher :
Page : 52 pages
File Size : 25,96 MB
Release : 1983
Category : Chlorides
ISBN :
Tabulation of discharge, chloride concentration, and chloride flux for the rivers and streams yields information related to heat flux from the park.
Recent Library Additions
Author :
Publisher :
Page : 472 pages
File Size : 28,92 MB
Release : 1990
Category : Engineering
ISBN :
Publications of the Geological Survey
Author : Geological Survey (U.S.)
Publisher :
Page : 456 pages
File Size : 37,20 MB
Release : 1990
Category : Geology
ISBN :
New Publications of the U.S. Geological Survey
Author : Geological Survey (U.S.)
Publisher :
Page : 462 pages
File Size : 19,34 MB
Release : 1994
Category : Geology
ISBN :
Anomalous Chloride Flux Discharges from Yellowstone National Park
Author : Irving Friedman
Publisher :
Page : 0 pages
File Size : 42,52 MB
Release : 1989
Category : Chlorides
ISBN :
The chloride concentration of some thermal springs in and adjacent to Yellowstone National Park is constant through time although their discharge varies seasonally. As a result the chloride flux from these springs increases during periods of increased discharge. We believe that this is caused by changes in the height of the local groundwater table, which affects the discharge of the springs but not their chloride concentration. The discharge from Mammoth Hot Springs varies seasonally, but its chloride concentration remains constant. We take this as evidence that this major thermal feature is derived from orifices that are tapping the local water table close to its surface. Three of the four major rivers (Yellowstone, Snake and Falls) exiting the Park also show an increased chloride flux during the spring runoff that cannot be explained solely by the contribution of snowmelt, nor by release of hot-spring-derived chloride stored in the soil during the winter and released in the spring. The increased chloride flux in these rivers is attributed to their draining shallow hot springs similar to those mentioned above. In contrast to the Yellowstone, Snake and Falls Rivers, the Firehole and Gibbon Rivers, which unite to form the Madison River and which collectively drain several major geyser basins, display a poor correlation between chloride flux and discharge. The cause, we believe, is that a large part of the thermal water input to these two rivers originated at great depths where the seasonal variation in the height of the water table had a negligible effect on hot spring discharge. Monitoring of seasonal discharge and chloride concentration of thermal features yields information on the depths at which these thermal features tap the local water table.