| 1. | Numerical simulation on groundwater seepage flow in the slope area of fissured rock
裂隙岩质边坡地下水渗流数值模拟 |
| 2. | The solid - liquid coupling theory of the groundwater seepage and the numerical method
地下水渗流的固液耦合理论及数值方法 |
| 3. | Effect of groundwater seepage on water and soil pressure in brace system of excavation
地下水渗流对基坑支护结构上水土压力的影响分析 |
| 4. | A new calculation chart of water - earth pressure on foundation pit considering groundwater seepage
考虑地下水渗流的基坑水土压力计算新图式 |
| 5. | Preliminary application of gms in simulation of groundwater seepage flowing field in dumping site in southeast of gushan iron mine
在姑山铁矿东南区排土场地下水渗流场的应用初探 |
| 6. | This thesis " s study has established a basis for studying consolidation , groundwater seepage and tunneling simulation
通过本论文的研究，可以为使用离心机研究固结沉降，地下水的渗流以及隧道模拟开挖打下基础。 |
| 7. | By analyzing and studying yujiaquan tail dam of luzhong mining group example , the failure , groundwater seepage arid dust nuisance of tail dam are studied
摘要通过分析研究鲁中冶金矿业集团的御驾泉尾矿序实例，对尾矿坝的破坏，尾矿库地下水渗漏和细粗尾矿库扬尘三个方面进行了研究。 |
| 8. | Effect of aquifer thickness , ratio of permeability coefficient and different aquifers on groundwater seepage and heat transfer caused by groundwater heat pump with pumping and recharging in the same well ( gwhpprsw ) is analyzed through numerical simulation
摘要模拟分析了含水层厚度、渗透系数比和不同含水层对同井回灌地下水源热泵地下水渗流和换热的影响。 |
| 9. | In analyzing the dynamic phenomenon in a groundwater for producing in type in different influence to take the foundation of the effect with characteristic and its environments , the influence mechanism for water matter activity to groundwater dynamic changes is studied , making use of theories the groundwater seepage flows and the water balance
在分析不同影响类型所产生的地下水动态的现象和特征及其环境负效应的基础上，利用地下水渗流和水均衡理论深入分析了水事活动对地下水动态的影响机理。 |
| 10. | Clustering figure shows that , along the route groundwater seepage , the melt water first recharges groundwater of nuoertu , then that of gurinai and guaizi lake ; the long clustering distances of groundwater samples of gurinai and guaizi lake perhaps result from infiltration of the heihe river ; it ' s impossible that water of heihe river recharges underwater of the badain jaran desert represented by nuoertu
由聚类图推测：祁连山冰川融水通过地下首先经过诺尔图，然后到达古日乃和拐子湖；古日乃和拐子湖地下水某些样品聚合距离大，可能是由黑河水渗入引起的，少量黑河水可通过古日乃渗入拐子湖引起地下水成分变化；没有迹象显示黑河水补给巴丹吉林沙漠（以诺尔图为代表）地下水。 |
