1) water-rock interaction
水岩作用
1.
Study on of the mechanism water-rock interaction of mine water from abandoned mines during infiltration through coal rock;
废弃煤矿矿井水在煤岩体入渗过程中的水岩作用机理研究
2.
Analysis on the Water-rock Interaction of Stilling Basin Slope of Nuozhadu Hydropower Station;
糯扎渡水电站溢洪道消力塘边坡水岩作用机理研究
3.
Experimental research on the time effect of water-rock interaction of the Mesozoic red bed in the Longquan area
龙泉山地区中生代红层水岩作用时效性实验研究
2) water-rock interaction
水-岩作用
1.
Geological and geochemical characteristics of water-rock interaction in the processes of uranium mineralization in Zhuguang-Xiazhuang uranium ore-concentrated district;
诸广-下庄铀矿集区成矿过程中水-岩作用的地质地球化学特征
2.
Based on the weak layer specimen taken from the dam site zone of Bapanxia hydropower station,the water-rock interaction tests are carried out in the saturated condition.
该文选取八盘峡水电站坝址夹层岩样在室内饱水状态下进行水-岩作用试验,试验时段内研究反应水溶液pH值和其中主要离子浓度的变化,结合夹层化学组分于试验前后的分析对比,探讨夹层组分的转化机制和液相组分随时间的动态演化规律。
3.
In this paper,a mathematical model is set up for reliability analysis of stochastic modeling for water-rock interaction (WRI).
依据化学热力学的基本原理,建立了一个由功能函数组成的数学模型来进行水-岩作用随机模拟的可信度分析。
3) water rock interaction
水-岩作用
1.
In this paper,a linear programming model of water rock interaction is established and is applied to the analysis and appraisal of complex hydrogeology condition of Xiluodu power station as an example from geochemistry.
采用水－岩作用热力学模拟的方法，以溪洛渡水电站工程为实例，从水化学方面对坝区复杂水文地质条件作了定量分析评价。
4) Water/rock interaction
水/岩作用
5) water-rock reactions
水-岩作用
1.
t is a new method of studying the water-rock reactions by modeling the reactions and calculating the amount of mineral dissolution between groundwater and rock by the means of liner programming.
采用线性规划的方法模似地下水与岩石之间的作用，计算地下水与岩石之间的矿物溶蚀量是水－岩作用研究的一个新方法。
6) water-rock reaction
水-岩作用
1.
Based on the comprehensions of Ordos Basin\' topography,landform,physiognomy,geotectonic cycle,rock-type,lithology and other characters,the chemical thermo-dynamics,mass action and mass conservation equations were used to simulate the water-rock reaction of groundwater in Ordos Cretaceous Basin by applying of hydrogeochemical integrated method and modeling technique.
在了解鄂尔多斯盆地的地形、地势、地貌、新构造运动、岩石类型、岩性构造和其他特征的基础上,运用化学热力学原理、质量作用定律和质量守恒定律,应用水文地球综合分析方法和地下水地球化学模拟技术,对白垩系洛河组地下水进行了水-岩作用的地球化学模拟。
2.
In this paper,as an example of Baihetan hydropower station engineering,a linear programming model of water-rock reaction is established,and complex hydrogeology condition in the dam area is quantitatively analyzed and evaluated from geochemistry aspect.
采用水-岩作用线型规划的模拟方法,以白鹤滩水电工程为实例,从水化学方面对坝区复杂水文地质条件作定量分析评价。
补充资料：水岩
水岩 端砚名坑之一。唐初开采，清道光十三年开坑时，岩洞塌方，自此便封坑不再开采，直至1972年才重新开坑采石。该坑自晚唐开始，采坑砚石所制之砚被列为贡品，故又称皇岩，清康熙后改称老坑。水岩砚石属泥质、硅质绢云母板岩，为变余泥质结构、粉砂质结构、隐晶质结构，平行构造。矿物成分为泥质、绢云母及硅质胶结而成，并含少量氢氧化铁，以及石英、白云母，电气石、锆石和绿泥石。水岩砚石呈紫蓝色，质地温软、幼嫩、细腻、滋润、致密、坚实，“体重而轻”、“质刚而柔”。具有“呵气研墨”、“贮水不耗”、发墨不损笔毫的特点，“叩之无声”、“磨墨亦无声”。水岩砚石的开采异常艰巨、复杂。水岩砚石在端砚名坑中，开采历史最长，石质最好，石品花式最多，研墨也最均匀，为世之珍品。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条