| 1. | Calculation and analysis of infiltration replenishment in river course
河道渗漏补给量的计算与分析 |
| 2. | Study of the precipitation infilatration recharge with the d , 18o isotopes peak displacement method
同位素峰值位移法求解大气降水入渗补给量 |
| 3. | ( 6 ) landscape ecology evaluation model has been established , selecting index from landscape structure and function and assessing the estate development action
量化生态功能的具体指标，为保证济南市泉域常年出流，研究区的地下水年补给量应达到1219万m ~ 3 。 |
| 4. | Aiming at the recharge capacity of rubber dam to the groundwater storage , the excited water supply of the dam caused by the exploitation of industry is discussed by mathematical simulation
并针对橡胶坝的补给能力，通过数值模拟探讨了坝内蓄水因工业开采而激发的补给量。 |
| 5. | Using numerical solution for inverse problem in partial differential equation , a method for initializing groundwater table on base one pumping test and recharge estimation on two pumping tests were presented . then a numerical model for groundwater table forecast was developed
本文利用对偏微分方程逆问题的数值求解，给出了由一组抽水井实测水位计算地下水初始水位以及由二组抽水井实测水位值估算总补给量的方法。 |
| 6. | Infiltration of atmosphetic water and river leakage are the major supply source of krast water in jinan spring field , while artificial water - taking and spring discharge are its major discharge forms . the karst water flows from south to north in the whole and the average recharge capacity is 55 x 104m3 / d
岩溶水补给来源主要为大气降水渗入和河流渗漏，排泄方式主要为人工开采和泉水排泄，总体向北径流，泉域多年平均补给量为55万m ~ 3 d 。 |
| 7. | Abstract : according to the base flow separation results from hydrographs in many watershed , the best regression equation expressing the relationship between annual precipitation infiltration coefficient and the weight of different strata area to total area of the watershed is established . the equation can be used to calculate the precipitation infiltration recharge for different ground water basins in which the strata distribution and the precipitation are given . the precipitation recharge is equivalent to the ground water recharge in some mountainous area where the exploitation of ground water resources are far from being sufficient
文摘:降水入渗补给系数与地层相关分析的目的，是为推求山丘区降水入渗补给量.鲁中山丘区是由各种不同地层出露组成的山丘区域.在多个水文流域基流分割基础上，建立流域年均降水入渗补给系数与各种地层出露面积占流域总面积权重间的最佳回归方程，利用该回归方程和地层分布及降水量推算不同地下水流域的降水入渗补给量.在地下水开发利用不高的山丘区，降水入渗补给量即为地下水补给量 |
| 8. | In the natural state , the confined water is mainly the palaeowater which was recharged in the past , and its circulation is slow ; but in the urban area where groundwater is exploited persistently , large volume of new water entered into the confined aquifer , and the rate of recharge from the upper aquifer accounts for 50 %
天然状态下，承压水为古地质时期补给形成的“古水” ，地下水交替缓慢；开采状况下，平原东部承压水受到了现代补给水的影响，潜水越流量占补给量的50 %左右。 |
| 9. | The water seepage from canal systems was one of the major factors in the analysis of water supply - demand balance . through the analysis of the monitoring data on water delivery in the canal systems , a generalized model of water loss at a unit length of canal and a mathematic model of canal percolation replenishment to the moving table of underground water were recommended
渠系渗漏是供需平衡分析过程中的一个主要因素，通过对渠系输水测试资料的分析研究，本文提出了单位长度渠系输水损失量的概化模型和变动水位条件下渠系渗漏补给量的数学计算模型。 |
| 10. | 2 . based on the analysis of the historical evolution of jinan springs ' spurting , a quantity equation between the anaual average spring discharge and the anaual lowest water table is built according to the statistic data , which enable us to gain the corresponding relation between baseline water level and the smallest scenic discharge of spring gushing . then the groundwater discharge in the spring area is calculated and the controlling parameter of maximum available amount of groundwater exploiting is obtained
泉域总面积1486平方公里。 (二)通过分析济南市泉群喷涌历史统计资料，首先建立泉群年平均喷涌量与年最低地下水位之间的定量方程，得出四大泉群喷涌的底限水位与最低景观流量的对应关系，然后，计算泉域内地下水的入渗补给量，再得出保证泉涌的地下水最大允许开采量的控制性参数。 |
