CONCENTRATIONS AND ACTIVITIES OF IONS IN SOLUTIONS DISPLACED FROM BASALTIC SOILS
CONCENTRATIONS AND ACTIVITIES OF IONS IN SOLUTIONS DISPLACED FROM BASALTIC SOILS
复制标题
从玄武岩土壤中置换出来的溶液中离子的浓度和活度
DOI：
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发表时间：
1977
期刊：
影响因子：
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通讯作者：
G. Fitzhugh
中科院分区：
文献类型：
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作者：
G. Benians;P. Scullion;G. Fitzhugh
总结
从安特里姆玄武岩土壤置换的土壤溶液进行了分析的主要无机成分。溶液中铝和磷酸盐几乎饱和，但硫酸盐未饱和。铁浓度大大超过氢氧化铁的溶解度。这些溶液的浓度低于英国和美国土壤中所描述的浓度，代表沥滤环境。
Summary
Soil solutions displaced from Antrim basaltic soils were analysed for major inorganic constituents. The solutions were nearly saturated with aluminium and phosphate but not sulphate. Iron concentrations were greatly in excess of ferric hydroxide solubility. The solutions were less concentrated than those described for soils of Britain and the U.S.A., representing a leaching environment.