喀斯特水

两城水源地喀斯特水资源评价

Assessment on Karst Water Resources of Water sources Area in Double-City

喀斯特水系统是由管流水与隙流水共同组成的水文地质系统，它们之间存在着复杂的耦合与转化关系。偏流作用引起夺水现象，进而导致汇流。

The system of karst water consists of conduit flow and diffuse flow ;

煤矿床裂隙喀斯特水突水通道特征

Characteristics of Crevice-karst Water Inrush Conduits in a Coal Deposit

主要的供水水源为中奥陶统碳酸盐类岩石中的裂隙-喀斯特水。

The main water source is fracture-karst water in Middle Ordovician carbonate rocks .

黔北高原喀斯特水的硬度特征

Hardness of karst water on North Guizhou Plateau

贵州喀斯特水资源集蓄利用模式研究

Research on the Collection Storage and Utilization Patterns of Karst Water Resources in Guizhou

关于喀斯特水系统研究

Research on karst water system

喀斯特水动力剖面模式反映各类水文地质结构中喀斯特水的埋藏、迳流条件和水动力特点。

The hydrodynamical section of karst reflects the conditions of karst water bury and runoff in var-ious hydrogeological structures as well as hydrodynamical characteristics .

并以断层为实例，给出了相应模型表示及其相应的集合运算，即集合间并、交、差等相关操作，从而生成三维煤矿床断层.煤矿床裂隙喀斯特水突水通道特征

Take the fault as an example , the representing and operation of model were put forward , then the 3D coal bed could be gained . Characteristics of Crevice-karst Water Inrush Conduits in a Coal Deposit

喀斯特地区水资源利用量可承载的GDP远高于其实际的GDP量；

The GDP that karst area can carry is higher than its realistic level of GDP .

基于TOPSIS法的喀斯特地区水资源承载力评价及演化探讨

The Assessment on the Water Resource Carrying Capacity Based on the Method of TOPSIS and a Discussion on Its Evolution in Karst Area

典型喀斯特流域水资源承载力研究

Study on Water Resources Carrying Capacity in Typical Karst Drainage

西南喀斯特山区水资源开发利用模式

The model of water resource utilization in karst area in Southwest China

基于指标权重的喀斯特地区水资源承载力评价

Assessment on Water Resources Carrying Capacity in Karst Area Based on Index Weight

喀斯特地区水下岩塞爆破的研究&印江岩口特大型山体滑坡应急整治工程水下岩塞爆破设计与分析

Study on Underwater Rock Plug Burst in Karst Area

喀斯特区域水安全评价理论与方法研究

Study on the Theory and Method of Water Safety Assessment in Karst Regions

贵州喀斯特地区水资源主要特征初步分析

Preliminary Analysis on Main Features of Water Resources in Karst Region of Guizhou Province

贵州喀斯特地区水资源存在问题及解决对策

The Problems and Strategies of Water Resource in the Karst Region in Guizhou Province

基于生态足迹法的喀斯特地区水资源承载能力综合评价研究

Comprehensive Assessment of Water Resource Carrying Capacity in Karst Area Based on Ecological Footprint Analysis

《贵州喀斯特地区水资源保护与高效利用技术开发与示范》项目研究工作阶段性总结

Phase Report on Exploration and Demonstration of Technology for Water Resource Conservation and its Efficiency Utilization

贵州喀斯特峡谷水保经济植物花椒土壤特性研究

Soil Characteristics of Zanthoxylum Bungeanum with Soil and Water Conservation Benefits in Karst Valley of Guizhou Province

基于主成分分析和熵的喀斯特地区水资源承载力动态变化研究&以贵阳市为例

A Study on the Evolution of Water Resource Carrying Capacity in Karst Area Based on Component Analysis and Entropy

结果表明，本区地下水有三个来源：深部喀斯特岩溶水、浅部孔隙水和地表水。

These results show that the underground water has three sources , namely deep karst , shallow porous and surface waters .

在水资源总量相当的情况下，一般喀斯特地区水资源承载力低于非喀斯特地区；

Generally , under the condition of the same water resources amount , the water resource carrying capacity in karst area is lower than non-karst area .

喀斯特峰林洼地水资源计算模型

A model of water resources computation for Karst pinnacles and depressions

山东临淄地区喀斯特&裂隙水资源的管理模型

On the management model of karst-fracture water resource in Linzi district , Shandong Province

喀斯特区域的水化学不稳定性&以黔中地区为例

Instability of Water Chemistry in the Karst Region & An Example from Central Guizhou

贵州省是典型的喀斯特省，水资源虽较为丰富，但可利用的、便于利用的水资源并不多。

Guizhou Province is a typical Karst provinces , although the more abundant water resources , but can be utilized to facilitate the use of water resources is not many .

引起塌陷的机理应是巨厚灰岩Ⅲ水动力带喀斯特管流水水动力场的变化，从而研究预防和治理措施也必须从这一主要方面入手，才能达到治本的效果。

The mechanism causing collapse should be the change of hydrodynamic field in the hydrodynamic zone ⅲ of the thick-bedded limestone , and the effect for permanent control of collapse could be achieved only when the prevention and harnessing measures are taken on the basis of this aspect .

论述了Au的矿源体（场）、特定的岩性和地质结构、挽近地史时期的气候和喀斯特地质结构和水动力系统在成矿中的内在联系及其对矿床分布的控制作用。

Discussion on the inherent relation in the ore-forming process of Au involving the original ore body , specific lithologic characters and geological structure , climate in neoid period and karst geological structure and hydrodynamic system and control process with deposit distribution has been carried out .