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电导率法
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  conductivity method
    DYNAMIC MONITORING OF GYPSUM DEHYDRATION PROCESS AT 0.5~1.5 GPa——ELECTRICAL CONDUCTIVITY METHOD
    0.5~1.5GPa下石膏脱水过程动态监测电导率法
短句来源
    degree of mineralization is an important index in the groundwater analysis In environmental monitoring,the conventional method to determine the degree of mineralization for groundwater is weighting method Through determining the Luoyang groundwater conductivity,analyzing the relationships between conductivity and mineralization rate,and establishing the quantitative relations between conductivity and mineralization rate by using regression equations We find out the indirect method for determining mineralization rate by conductivity method The advantages for conductivity method are speedy,economical and accurate
    其缺点主要为费时,繁琐,耗电。 本文通过测定洛阳市地下水的电导率,分析对比电导率与矿化度的关联,并进一步用回归方程确定电导率与矿化度之间的数量关系,探索出用电导率法间接测定地下水矿化度,具有快速,经济,准确的优点。
短句来源
    Electrical conductivity method can be used to monitor dynamically the dehydration process of hydrous minerals, and to study the distribution and migration kinetics of free water.
    电导率法是适用于含水矿物脱水过程动态监测及脱水过程中水的分布、迁移等动力学过程就位研究的有效方法。
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    The EH 4 continuous resistivity method was used to explore the Ye'erya gold orefield along 16 28 lines. The preliminary analysis and interpretation have revealed the distribution and shape of the deep granite body. The granite body strikes westward.
    运用EH 4连续电导率法对峪耳崖金矿区 16 2 8线进行测量 ,通过初步的分析解译 ,基本确定了深部花岗岩体的分布范围和形态 ,大致了解了岩体向西的展布特征。
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  conductivity method
The calculated transpiration of the Populus euphratica canopy was 214.9 mm based on the specific conductivity method.
      
Using the local electrical conductivity method, the parameters of the linear waves generated on the surface of a falling liquid film in the presence of a co- or counter-current gas stream are measured.
      
The kinetics of collective recrystallization in Sn-Pb, Sn-In, Sn-Zn, Pb-Sn, Pb-Bi, and Pb-In alloys have been studied using the conductivity method at T = 180°C.
      
The electric conductivity of pollen life-force and male flowers ofLarix olgemis on condition of low temperature adversity has been respectively measured by means of fluorescent dying method and conductivity method in 1992 and 1994.
      
Dehydration temperature of serpentine at elevated temperatures and pressures by electrical conductivity method and its implicati
      
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On the abnomalous isopleth, the proximal points and distal points of drainage can be identified from the anomalous contents of elements for each sampling point. The two kinds of sampling points with different contents of elements are connected to form proximal area with nonisopleth( the anomalous area is reduced to 1/2 or 2/3 ). The anomalous source is traced by the principle that microelectrical anomaly is consistent with secondary anomaly in soil electrical conductivity. A few geochemical prospecting samples...

On the abnomalous isopleth, the proximal points and distal points of drainage can be identified from the anomalous contents of elements for each sampling point. The two kinds of sampling points with different contents of elements are connected to form proximal area with nonisopleth( the anomalous area is reduced to 1/2 or 2/3 ). The anomalous source is traced by the principle that microelectrical anomaly is consistent with secondary anomaly in soil electrical conductivity. A few geochemical prospecting samples are combined to locate the anomalous source.

在异常等值线内,从各采样点的元素异常含量,分辩出异常源经过水系时的近源点与远源点,用非等浓度线将这些元素含量各不相同的两类点连成近源区(缩小异常面积1/2至2/3以上),然后在此区内应用土壤电导率法的微电性异常与化探次生异常具有一定同源性的原理,追踪异常源,并用少量化探样品做配合,提供异常出露的位置。

degree of mineralization is an important index in the groundwater analysis In environmental monitoring,the conventional method to determine the degree of mineralization for groundwater is weighting method Through determining the Luoyang groundwater conductivity,analyzing the relationships between conductivity and mineralization rate,and establishing the quantitative relations between conductivity and mineralization rate by using regression equations We find...

degree of mineralization is an important index in the groundwater analysis In environmental monitoring,the conventional method to determine the degree of mineralization for groundwater is weighting method Through determining the Luoyang groundwater conductivity,analyzing the relationships between conductivity and mineralization rate,and establishing the quantitative relations between conductivity and mineralization rate by using regression equations We find out the indirect method for determining mineralization rate by conductivity method The advantages for conductivity method are speedy,economical and accurate

矿化度是地下水化学成份测定的重要指标,在环境监测中,用重量法测定矿化度是目前普遍采用的方法。其缺点主要为费时,繁琐,耗电。本文通过测定洛阳市地下水的电导率,分析对比电导率与矿化度的关联,并进一步用回归方程确定电导率与矿化度之间的数量关系,探索出用电导率法间接测定地下水矿化度,具有快速,经济,准确的优点。

Dehydration process of gypsum was monitored by measuring the variation of electrical conductivity with time dynamically at 0.5~1.5 GPa and 160~255℃. The results showed that the variation of electrical conductivity with time during dehydration may involve two stages. The variation of electrical conductivity with time during the first stage can reflect indirectly the rates of dehydration reaction. Variations during the second stage reflect the increasing concentrations of the dissolved ions in fluids. Variations...

Dehydration process of gypsum was monitored by measuring the variation of electrical conductivity with time dynamically at 0.5~1.5 GPa and 160~255℃. The results showed that the variation of electrical conductivity with time during dehydration may involve two stages. The variation of electrical conductivity with time during the first stage can reflect indirectly the rates of dehydration reaction. Variations during the second stage reflect the increasing concentrations of the dissolved ions in fluids. Variations in phase angles with time can reflect dynamically the existence and connectivity of dehydrated free water. Electrical conductivity method can be used to monitor dynamically the dehydration process of hydrous minerals, and to study the distribution and migration kinetics of free water.

在 0 .5~ 1 .5GPa,1 60~ 2 55℃条件下动态监测了石膏脱水过程中电导率随时间的变化。实验结果表明 ,脱水过程中电导率随时间的变化分两个阶段 :第一阶段电导率随时间的变化速率可间接地反映脱水反应的速率 ;第二阶段反映了流体中溶解离子的增多。相角随时间的变化可动态反映释放的水在矿物颗粒边缘的存在及连通性。电导率法是适用于含水矿物脱水过程动态监测及脱水过程中水的分布、迁移等动力学过程就位研究的有效方法。

 
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