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Record #125793:

Hydrologic and water quality characteristics of a degrading open-system pingo / Charles W. Slaughter, Ronald J. Hartzmann.

Title: Hydrologic and water quality characteristics of a degrading open-system pingo / Charles W. Slaughter, Ronald J. Hartzmann.
Author(s): Slaughter, Charles W.
Hartzmann, Ronald J.
Date: 1993.
Publisher: Wushan, Guangzhou: South China University of Technology Press
In: Permafrost. Sixth International Conference. Proceedings (Vol. 1), July 5-9, 1993, Beijing China. (1993.),
Abstract: Reports observations of pingo in discontinuous permafrost zone of Yukon-Tanana uplands of central Alaska over four summer seasons. Water discharge was not responsive to summer precipitation and did not appear related to ambient air temperature. Chemistry of pingo outflow was consistently different from and apparently unrelated to chemistry of streamflow in adjacent stream. Suggests that water from this pingo is derived from subpermafrost groundwater, initially infiltrated at higher elevations.
Notes:

In: Permafrost. Sixth International Conference. Proceedings (Vol. 1), July 5-9, 1993, Beijing China / International Conference on Permafrost.

Keywords: 551.34 -- Geocryology. Frozen ground.
551.343.72 -- Frost mounds. Pingos.
556 -- Hydrology.
E11 -- Glaciology: glaciohydrology.
(*49) -- Alaska.
(*493) -- Alaska, interior.
SPRI record no.: 125793

MARCXML

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100 1# ‡aSlaughter, Charles W.
245 10 ‡aHydrologic and water quality characteristics of a degrading open-system pingo /‡cCharles W. Slaughter, Ronald J. Hartzmann.
260 ## ‡aWushan, Guangzhou :‡bSouth China University of Technology Press,‡c1993.
300 ## ‡ap. 574-579 :‡bdiags.
500 ## ‡aIn: Permafrost. Sixth International Conference. Proceedings (Vol. 1), July 5-9, 1993, Beijing China / International Conference on Permafrost.
520 3# ‡aReports observations of pingo in discontinuous permafrost zone of Yukon-Tanana uplands of central Alaska over four summer seasons. Water discharge was not responsive to summer precipitation and did not appear related to ambient air temperature. Chemistry of pingo outflow was consistently different from and apparently unrelated to chemistry of streamflow in adjacent stream. Suggests that water from this pingo is derived from subpermafrost groundwater, initially infiltrated at higher elevations.
650 07 ‡a551.34 -- Geocryology. Frozen ground.‡2udc
650 07 ‡a551.343.72 -- Frost mounds. Pingos.‡2udc
650 07 ‡a556 -- Hydrology.‡2udc
650 07 ‡aE11 -- Glaciology: glaciohydrology.‡2local
651 #7 ‡a(*49) -- Alaska.‡2udc
651 #7 ‡a(*493) -- Alaska, interior.‡2udc
700 1# ‡aHartzmann, Ronald J.
773 0# ‡7m2am ‡aInternational Conference on Permafrost. ‡tPermafrost. Sixth International Conference. Proceedings (Vol. 1), July 5-9, 1993, Beijing China. ‡dWushan, Guangzhou : South China University of Technology Press, 1993. ‡wSPRI-125499
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