1) rich H2 fluid
富H流体
1.
Under the high oxygen fugacity condition, the fluid is composed of CO2+H2O (rich CO2 fluid); under the low oxygen fugacity, the fluid is composed of CH4+H2+H2O(rich H2 fluid).
深部流体是影响油气形成的一个重要因素,根据进入盆地的深部流体的化学组分与同位素特征,可以把深部流体分为两种组合类型,高氧逸度环境下,以CO2+H2O为主成分(富CO2流体);低氧逸度的流体,主要组分为CH4+H2+H2O(富H流体)。
2) potassic-rich fluid
富钾流体
3) germanium-enriched fluid
富锗流体
1.
The result shows that the coal seams are a kind of country rock extremely favorable to germanium mineralization,and whether the coal is able to enrich in germanium depends principally on whether or not there exists germanium-enriched fluid which can interact with the coal.
结果表明，煤是锗成矿极有利的围岩，煤能否富集锗主要取决于有无富锗流体与煤相互作用。
4) F rich fluid
富氟流体
5) aqueous fluid
富水流体
1.
The aqueous fluid in subduction zone has played important role for the evolution of crust and mantle and the mass exchange.
重点剖析:1)超临界态下温度压力条件的改变导致水微观结构与性质的变化,扩散系数、粘度等性质随之改变,进而对水岩反应产生影响;2)富水流体中离子缔合影响着金属配合物数量,很大程度制约流体中矿物的溶解行为;3)低Cl流体中微量元素配分模式与岛弧玄武岩类似,意味着富水贫氯碱性硅酸盐成分的流体在地幔楔元素运移中起关键作用。
6) rich CO2 fluid
富CO2流体
1.
Under the high oxygen fugacity condition, the fluid is composed of CO2+H2O (rich CO2 fluid); under the low oxygen fugacity, the fluid is composed of CH4+H2+H2O(rich H2 fluid).
深部流体是影响油气形成的一个重要因素,根据进入盆地的深部流体的化学组分与同位素特征,可以把深部流体分为两种组合类型,高氧逸度环境下,以CO2+H2O为主成分(富CO2流体);低氧逸度的流体,主要组分为CH4+H2+H2O(富H流体)。
补充资料：过氧化单硫酸钾与硫酸二钾和硫酸氢钾的化合物
CAS：37222-66-5
中文名称：过氧化单硫酸钾与硫酸二钾和硫酸氢钾的化合物
英文名称：Peroxymonosulfuric acid, monopotassium salt, mixture with dipotassium sulfate and potassium hydrogen sulfate； potassium peroxymonosulfate sulfate,(2khso5.khso4.k2so4)； Peroxymonosulfuric acid,monopotassium salt,mixture with dipotassium sulfate and potassium hydrogen sulfate
中文名称：过氧化单硫酸钾与硫酸二钾和硫酸氢钾的化合物
英文名称：Peroxymonosulfuric acid, monopotassium salt, mixture with dipotassium sulfate and potassium hydrogen sulfate； potassium peroxymonosulfate sulfate,(2khso5.khso4.k2so4)； Peroxymonosulfuric acid,monopotassium salt,mixture with dipotassium sulfate and potassium hydrogen sulfate
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