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Chemical weathering in high‐sediment‐yielding watersheds, New Zealand
Author(s) -
Lyons W. Berry,
Carey Anne E.,
Hicks D. Murray,
Nezat Carmen A.
Publication year - 2005
Publication title -
journal of geophysical research: earth surface
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2003jf000088
Subject(s) - denudation , erosion , weathering , sediment , yield (engineering) , geology , hydrology (agriculture) , environmental science , geomorphology , materials science , geotechnical engineering , metallurgy , paleontology , tectonics
We have determined the chemical erosion yields for fifteen watersheds in New Zealand, ranging in size from 12.2 to 2928 km 2 . These rates, coupled with previously measured physical erosion yields, allow us to compare these two modes of landscape denudation. The physical erosion yields are some of the highest measured in the world. Although in most instances the chemical erosion yields are only a small fraction of the total erosion yields, the absolute values are very high. Our data strongly support the notion that chemical erosion rates are greatly influenced by the yield of physical erosion and that the rapid production of fresh surfaces as a result of high physical erosion rates and subsequent denudation is critical to the high chemical erosion yields observed.

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