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Geochemical evolution of high-pH sodic salt pans in Central Otago, New Zealand
New Zealand Journal of Geology and Geophysics ( IF 1.9 ) Pub Date : 2022-05-19 , DOI: 10.1080/00288306.2022.2076701 Dave Craw 1 , Cathy Rufaut 1 , Dhana Pillai 1 , Gemma Kerr 1
New Zealand Journal of Geology and Geophysics ( IF 1.9 ) Pub Date : 2022-05-19 , DOI: 10.1080/00288306.2022.2076701 Dave Craw 1 , Cathy Rufaut 1 , Dhana Pillai 1 , Gemma Kerr 1
Affiliation
Soil-free sodic salt pans with local pH >10 have formed on loess and schist-derived clay surfaces in the semi-arid climate of Central Otago. This study identifies evaporative mineral distributions ...
中文翻译:
新西兰中奥塔哥高 pH 钠盐田的地球化学演化
在中奥塔哥的半干旱气候中,黄土和片岩粘土表面形成了局部 pH >10 的无土钠盐田。这项研究确定了蒸发矿物分布......
更新日期:2022-05-19
中文翻译:
新西兰中奥塔哥高 pH 钠盐田的地球化学演化
在中奥塔哥的半干旱气候中,黄土和片岩粘土表面形成了局部 pH >10 的无土钠盐田。这项研究确定了蒸发矿物分布......