Prediction of limestone solution rates from rainfall and runoff data: Some comments
Prediction of limestone solution rates from rainfall and runoff data: Some comments
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根据降雨和径流数据预测石灰石溶解率：一些评论
DOI：
10.1002/esp.3290060609
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发表时间：
1981
影响因子：
3.3
通讯作者：
J. Gunn
中科院分区：
文献类型：
--
作者：
J. Gunn
Lang（1977）最近关于石灰岩流域中与降雨有关的溶解侵蚀速率的研究存在严重错误，其逻辑基础也有问题。尽管Smith和Atkinson（1976年）关于径流侵蚀率的研究要合理得多，但也需要修改，因为它大大高估了新西兰两个地区的侵蚀率。通过将自生径流与自生沃茨的溶解速率联系起来，并通过计算在开放和封闭系统平衡条件下发生溶解的区域的单独关系，可能会获得更高的分辨率。这些因素应在未来研究的实验设计中加以考虑。
Recent work by Lang (1977) on solutional erosion rates in limestone drainage basins in relation to rainfall contains serious errors and has a questionable logical basis. Although much sounder, Smith and Atkinson's (1976) work on erosion rates in relation to runoff also requires modification as it greatly overestimates erosion rates in two areas of New Zealand. Greater resolution could probably be obtained by relating autogenic runoff to the rate of solution by autogenic waters and by computing separate relationships for areas where solution takes place under open and closed system equilibrium conditions. These factors should be taken into account in the experimental design of future studies.