矿物水体系氢同位素平衡分馏系数和动力分馏系数是同位素地球化学研究中的重要参数。
The hydrogen isotope equilibrium fractionation factors and kinetic fractionation parameters are the important basic data for the study of isotope geochemistry.
金属矿物硫同位素组成在同位素交换平衡条件下属中低温环境沉淀。
The s isotopic components of metal minerals indicates a mid-low-temperature environmental precipitation under the condition of isotopic exchange equilibrium.
固体表面吸附的氢同位素具有自发与气相氢同位素交换并达到某种程度平衡的性质，这种交换作用在金属氢化物表面同样存在。
The hydrogen absorbed on solid surface can exchange with its isotopes in gas phase until equilibrium achieved. Such characteristic exists in metal hydride-hydrogen system, too.
碳酸盐岩风化对碳平衡和锶同位素变化的影响不可被忽视。
The results report here reveal more evidence for CO2 comsumption and the evlution of Sr isotope by carbonate weathering.
碳酸盐岩风化对碳平衡和锶同位素变化的影响不可被忽视。
The results report here reveal more evidence for CO2 comsumption and the evlution of Sr isotope by carbonate weathering.
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