INDEX OF WEATHERING FOR SILICATE ROCKS
INDEX OF WEATHERING FOR SILICATE ROCKS
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DOI：
10.1017/s0016756800058581
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发表时间：
1970-01-01
影响因子：
2.3
通讯作者：
PARKER, A
中科院分区：
文献类型：
--
作者：
PARKER, A
根据存在的碱金属和碱土金属的比例，提出了硅酸盐岩石的风化指数。这些被认为是最具流动性的主要元素。元素与氧的结合强度被用作该指数的权重因子，该指数既衡量了岩石相对于母质已经风化的程度，也衡量了其进一步风化的敏感性。
An index of weathering for silicate rocks is proposed, based on the proportions of the alkali and alkaline earth metals present. These are considered to be the most mobile of the major elements. The bond strengths of the elements with oxygen are used as weighting factors in the index, which measures both the degree to which a rock has already been weathered with respect to the parent material, and also its susceptibility to further weathering.