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涌水
相关语句
  water inrush
    Based on analysis of hydrogeological condition of Huize lead-zinc ore deposit,the water volume contained in aquifer of the deposit is estimated by means of equivalent fracture medium model. Besides,with the help of information about stope's water inrush and the help of survey of deposit's underground water level,the possible water inrush at 1 511 and 1 451 levels of Qilinkeng ore body is predicted using Ritz Finite Element Method.
    通过对会泽铅锌矿区水文地质条件的研究 ,采用等效裂隙介质模型概化矿床充水含水层 ,并利用矿坑涌水资料及矿区地下水水位观测资料 ,应用里兹 (Ritz)有限单元法计算和预测了麒麟厂矿坑深部 15 11、 145 1m两个中段的涌水量。
短句来源
  water in rush
    Based on analysis of hydrogeological condition of Huize lead-zinc ore deposit,the water volume contained in aquifer of the deposit is estimated by means of equivalent fracture medium model. Besides,with the help of information about stope's water inrush and the help of survey of deposit's underground water level,the possible water inrush at 1 511 and 1 451 levels of Qilinkeng ore body is predicted using Ritz Finite Element Method.
    通过对会泽铅锌矿区水文地质条件的研究 ,采用等效裂隙介质模型概化矿床充水含水层 ,并利用矿坑涌水资料及矿区地下水水位观测资料 ,应用里兹 (Ritz)有限单元法计算和预测了麒麟厂矿坑深部 15 11、 145 1m两个中段的涌水量。
短句来源
  “涌水”译为未确定词的双语例句
    AN APPLIED STUDY ON PREVENTION OF WATER BURSTING DISASTER IN MINES WITH THE HIGH RESOLUTION V6 SYSTEM
    高分辨V6系统在矿山顶板涌水隐患中的应用研究
短句来源
    Anclysis of mine water source Jinchiling gold mine
    金翅岭金矿矿床涌水来源分析
短句来源
    The technology for prediction of water in flow disasters in long and large tunnel, karst areas
    岩溶地区长大隧道涌水灾害预测预报技术
    THE CONNECTING EXPERIMENTAL STUDY ON KARST WATER-IN-FLOW IN DAYAOSHAN TUNNEL
    大瑶山隧道岩溶涌水的连通试验研究
短句来源
    THE FEATURES OF GEOMORPHOLOGY AND NEOTECTONIC MOVEMENT IN LIUJIANG BASIN AND THE IMUENCES ON PIT WATER YIELD OF COAL MINE
    柳江盆地地貌与新构造运动特征及其对煤矿坑道涌水的影响
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  water inrush
Hundreds of water inrush accidents have occurred and over 30 mines have been flooded, resulting in heavy economic losses and casualties.
      
Hundreds of water inrush incidences have occurred in which a large amount of water suddenly flows into tunnels or working faces under high potentiometric pressure and over 30 mines have been flooded over the last 20?years.
      
When the water pressure in the underlying aquifer exceeds Phf, a wedging effect takes place within the fractures of the geological barrier and, as a result, water inrush occurs.
      
Based on the test results, a new safety criterion for water inrush was derived for mines and it has been successfully applied to mining practices with the minimum effort of dewatering in the karst aquifer.
      
Water inrush and environmental impact of shallow seam mining
      
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There are two kinds of ground hot water in Wulongbei hot spring. One existing in estimated hot structure is named “deep circulative hot water”, the other existing in the crusk of bed rock is named “shallow circulative hot water”.Water temperature of the “deep circulative hot water” is higher than 60℃, artesian water, positive head are higher than 4m., hydraulic discharge is bigger than 0.2l/s.m, and the contain of F (Ⅰ) , Na (Ⅰ) , SiO_2, CO_3 (Ⅱ) , SO_4 (Ⅱ) are high. Water quality belongs to C.H-N type, water...

There are two kinds of ground hot water in Wulongbei hot spring. One existing in estimated hot structure is named “deep circulative hot water”, the other existing in the crusk of bed rock is named “shallow circulative hot water”.Water temperature of the “deep circulative hot water” is higher than 60℃, artesian water, positive head are higher than 4m., hydraulic discharge is bigger than 0.2l/s.m, and the contain of F (Ⅰ) , Na (Ⅰ) , SiO_2, CO_3 (Ⅱ) , SO_4 (Ⅱ) are high. Water quality belongs to C.H-N type, water temperature is not influenced by seasonal temperature.Water temperature of the “shallow circulative hot water” is lower than 60℃, spring is weak, hydaulic discharge is smaller than 0.11/s.m, and the contain of HCO_3 (Ⅰ) , Ca (Ⅱ) , Mg (Ⅱ) ,K (Ⅰ) are high. Water quality belongs to H—N type, water temperature is influenced by seasonal temperature.Water temperature of two kinls of ground hot water correlate with each other. Hydraulic relation is weak,and perhaps they are two independent hot water circul ative system.“Deep circulative hot water” is controlled by estimated hot structure, recharge of atmospheric precipitation. Hot source may be ground temperature field that is formed by radioactive heat. Hot source of the “shallow circulative hot water” is connected with heating action of the “deep circulative hot water”.

五龙背温泉地下热水有两种类型——赋存于热储构造中的“深循环型热水”和赋存于基岩裂隙中的“浅循环型热水”。“深循环型热水”的水温大子60℃;多为自流水;正水头大于4m;单位涌水量大于0.21/s.m;水质类型以C·H—N型为主,F~-、Na~+、SiO_2、CO_3~(2-)、SO_4~(2-)含量高,水温不受季节性气温影响。“浅循环热水”的水温小于60℃;有微弱涌水现象;单位涌水量小于0.11/s.m;水质类型为H—N型;HCO_3~-、Ca~(2+)、Mg~(2+)、K~+含量高;水温受季节性气温制约。两种类型地下热水水温具相关关系,水力联系微弱,两者可能为基本独立的水热循环系统。“深循环型热水”受热储构造控制,由区域大气降水补给,热源可能为放射性元素衰变所释放的能量而形成的地温场。“浅循环型热水”与基岩裂隙水成因相同,热源与“深循环型热水”加热作用有关。

The presentpaper givessome new ideas about the prediction of tunnel inflow in karst area and, in particular, in the vertical percolating zoneby the method of water balance. It stresses 'the discussion on catchment area and infiltration capacity watershed area; non-linear relationship between rainfall and infiltration capacity; critical rainfall; non-linear characteristics of percolation factor; interrelation of percolation amount and tunnel inflow: inflow coefficient; and computation and segmentation of tunnel...

The presentpaper givessome new ideas about the prediction of tunnel inflow in karst area and, in particular, in the vertical percolating zoneby the method of water balance. It stresses 'the discussion on catchment area and infiltration capacity watershed area; non-linear relationship between rainfall and infiltration capacity; critical rainfall; non-linear characteristics of percolation factor; interrelation of percolation amount and tunnel inflow: inflow coefficient; and computation and segmentation of tunnel inflow.

本文对水均衡法预测岩溶区(特别是垂直渗流带内)坑道涌水量问题提出了一些新的见解。文章着重讨论了:集水面积与汇水面积,降雨量与入渗量的非线性关系和临界降雨量,入渗系数的非线性特征,入渗量与坑道涌水量的关系和涌水系数,坑道涌水量的计算与分段等。

Study of the ground water gush in the juncture of liaoning and jilin province in 1987 shows that the big sum of rain fall in the autumn of 1988 and the cold wheather are the main reasons for the water gush. in autumn, the shallowuncenfined aquifer was full saturated, and upper of the aquifer became frozen and formed an impermanent irnpermeable layer, the volume of the frozen pert increased, and an additional pressure applied to the lower apuifer led to that that the ground water was under pressure. As temperature...

Study of the ground water gush in the juncture of liaoning and jilin province in 1987 shows that the big sum of rain fall in the autumn of 1988 and the cold wheather are the main reasons for the water gush. in autumn, the shallowuncenfined aquifer was full saturated, and upper of the aquifer became frozen and formed an impermanent irnpermeable layer, the volume of the frozen pert increased, and an additional pressure applied to the lower apuifer led to that that the ground water was under pressure. As temperature rised, the thin-frozen part melted, the ground watts under pressure gushed out. This phenomenon disappeared with the thawing of frozen soil.study of 15 wells in jilin and the juncture of Liaoning and Jilin province gives a background of the water level changes . it is believed that the long-term decrease of water table in Jiaohe well and the long term increase in siping well were in normal state and hat little relation with tectonic stress.

本文首先对1987年冬春在吉辽蒙交界地区出现的大面积地下涌水现象进行了分析。认为:该区因1986年秋季大量集中降雨,使浅层地下水极度饱和,冬季上层冻结暂时变成隔水层,同时给下层以巨大的冻胀负荷压力成为承压状态,当温度稍高时,在薄弱部位形成岛状融化,下层水夺路而出,造成涌水现象,此现象随冻土层的消融而消失。其次,通过吉林省及辽吉蒙地区15口井,对区域地下水动态进行分析,特别对蛟河井水位趋势下降和四平井水位趋势上升进行重点解剖、认为该区井水位基本处于正常动态阶段,与区域构造活动关系不大。

 
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