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Hillslope hydrology in a small fores...
~
Brammer, Dean Derek.
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Hillslope hydrology in a small forested catchment, Maimai, New Zealand.
紀錄類型:
書目-電子資源 : Monograph/item
正題名/作者:
Hillslope hydrology in a small forested catchment, Maimai, New Zealand./
作者:
Brammer, Dean Derek.
面頁冊數:
153 p.
附註:
Source: Masters Abstracts International, Volume: 35-01, page: 0185.
Contained By:
Masters Abstracts International35-01.
標題:
Hydrology. -
電子資源:
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1382126
ISBN:
0591156512
Hillslope hydrology in a small forested catchment, Maimai, New Zealand.
Brammer, Dean Derek.
Hillslope hydrology in a small forested catchment, Maimai, New Zealand.
- 153 p.
Source: Masters Abstracts International, Volume: 35-01, page: 0185.
Thesis (M.S.)--State University of New York College of Environmental Science and Forestry, 1996.
Integrated hydrometric and chemical tracing experiments were conducted at the Maimai Catchment, New Zealand to determine the relative importance of surface vs. bedrock topography in controlling water movement downslope. A hillslope in the M8 catchment was instrumented with a grid of suction lysimeters and maximum-rise wells. A pre-existing subsurface flow collection system was used to measure continuous flow across a trench face at the base of the hillslope. Surface and bedrock topography were surveyed for the entire slope. A line source of LiBr was applied upslope of the instrumented hillslope grid. The movement of tracer was tracked downslope through the grid and off slope at the trench face. Lateral preferential movement of tracer water to less mobile regions of the hillslope at the soil-bedrock interface was detected. These waters were re-mobilized by subsequent rainfall inputs. Results indicate that bedrock topography and soil depth variation are the dominant controls on the downslope movement of water and solutes at the hillslope scale in this steep humid catchment.
ISBN: 0591156512Subjects--Topical Terms:
545716
Hydrology.
Hillslope hydrology in a small forested catchment, Maimai, New Zealand.
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Integrated hydrometric and chemical tracing experiments were conducted at the Maimai Catchment, New Zealand to determine the relative importance of surface vs. bedrock topography in controlling water movement downslope. A hillslope in the M8 catchment was instrumented with a grid of suction lysimeters and maximum-rise wells. A pre-existing subsurface flow collection system was used to measure continuous flow across a trench face at the base of the hillslope. Surface and bedrock topography were surveyed for the entire slope. A line source of LiBr was applied upslope of the instrumented hillslope grid. The movement of tracer was tracked downslope through the grid and off slope at the trench face. Lateral preferential movement of tracer water to less mobile regions of the hillslope at the soil-bedrock interface was detected. These waters were re-mobilized by subsequent rainfall inputs. Results indicate that bedrock topography and soil depth variation are the dominant controls on the downslope movement of water and solutes at the hillslope scale in this steep humid catchment.
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http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1382126
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