補給地下水 的英文怎麼說

中文拼音 [bǔgěidexiàshuǐ]
補給地下水 英文
recharging groundwater
  • 補 : Ⅰ動詞1 （修理; 修補） repair; mend; patch 2 （補充; 補足;填補） fill up; add supplement; supply; ...
  • 給 : 給Ⅰ動詞1 （送對方某物; 使對方得到） give; grant 2 （用在動詞后 表示交與 付出） pass; pay 3 （叫; ...
  • 下 : 下動詞1. （用在動詞后,表示由高處到低處） 2. （用在動詞后, 表示有空間, 能容納） 3. （用在動詞后, 表示動作的完成或結果）
  • 水 : 名詞1 （由兩個氫原子和一個氧原子結合而成的液體） water 2 （河流） river 3 （指江、河、湖、海、洋...
  • 補給 : supply; provision; fitting out; replenishment; feed; recharge
  1. In order to control the land subsidence, adjusting three dimensional exploitive positions and moderately utilizing the leakage recharge from its upper shallow groundwater play a key role in realizing the sustainable development of deep groundwater resources in this area

    在控制地面沉降的條件下，深層地下水持續利用的對策是調整開采三維布局，適度開發利用淺層地下水對深層地下水的越流補給。
  2. This article analyzes the mineralization mechanism of the uranium ore, constructs a series of spectra indexes including the ferric oxide index, the ferrous oxide index, the oxidation index, clay mineral index, brightness index, the green index and the humidity index, and draws the distribution and scope of the oxidation belt, deoxidation belt, the supplies and partial drainage of ground water in the research area, thus selects the advantageous area of uranium mineralization

    通過分析鈾礦的成礦機理，構建了氧化鐵指數、氧化亞鐵指數、氧化指數、粘土礦物指數、亮度指數、綠度指數和濕度指數等一系列光譜指數，提取了研究區氧化帶、還原帶、地下水補給與局部排泄的分佈和范圍，從而圈定了鈾礦成礦的有利區。
  3. The agency will require the right to spread surface water, including reclaimed wastewater for ground water recharge.

    為了地下水人工補給，該機構需有引滲地表水（包括已回收的廢水）之權。
  4. There are two water cycle systems that are mutual independence and interaction, receiving provision from yeerqiang river and tizinapu river

    流域分為兩個相互獨立而又相互影響的地下水循環系統，分別接受葉河、提河水補給。
  5. ( 3 ) dynamic state of groundwater in riverside displays : at middle and supreme areas of yeerqiang, no matter abundant water season or low water season, river water always recharge groundwater. at downsteam, in abundant water season, river water recharge groundwater ; in low water season groundwater recharge the river

    （ 3 ）近河岸地帶地下水動態分析顯示葉爾羌河中上游地區，無論豐水季節還是枯水季節，河水均補給地下水：下游地區，豐水季節，河水補給地下水；枯水季節，地下水補給河水。
  6. Article 45 artificial recharge for ground water may not deteriorate the quality of ground water

    第四十五條人工回灌補給地下水，不得惡化地下水質。
  7. Management of aquifer recharge for sustainability : summary of the 4th international symposium on artificial recharge of groundwater

    第四屆國際地下水人工補給會議綜述
  8. The over - exploited deep confined water, which is replenished by surface water and phreatic water, is also polluted

    由於大規模開采，深層承壓水受到地表水和淺層地下水的補給，水質也有污染。
  9. On this basis, it also studies the main recharge of groundwater, discusses the relationships between river and groundwater, shallow confined water and phreatic water, northern karst water and quaternary phreatic water as well, and get the recharge percentage which river recharges to phreatic water

    在此基礎上，研究了地下水的補給來源，探討了河水與地下水、淺層承壓水與潛水、北部巖溶水與山前第四紀潛水之間的相互關系，確定了河水對潛水的補給比例。
  10. Aiming at this question, the paper put forward utilizing layer of soil to depurating rainwater project. the paper researches the rule of soil depurating rainwater and ascertain measure of cortroling contamination, on the basis of which the paper put forward rainwater depurated by soil to manual recharging groundwater project

    針對這一問題，本文提出就地利用土壤層收集凈化雨水的方案，研究了雨水在土壤層中的凈化規律，確定需要採取的污染控制措施，並在此基礎上以西安市某規劃小區為例，提出雨水通過土壤層凈化後人工補給地下水的實施方案。
  11. To this area precipitation materials for many years, evaporate materials, surface flow materials, hydrometeorological materials, hydrogeological materials carry on exhaustive analysis, have analysed the state of water resource of the sand district, proceed from the heat of the earth ' s surface is balanced, water yield balanced basic theories, combine the amount of regional water resource set up of the materials, such as scene, hydrology, soil of the sand district, etc. and estimate models, have calculated the surface water, groundwater of this area, has carried on models to examine according to the real data, and has predicted to the state of water resource under different climate change scenes of future that analyse. have put forward the scheme that the water resource in this area utilized rationally, use the non - linear motive force model to predict the precipitation, utilize the materials of actual observation, the natural supply amount of calculating out groundwater of sand ground of balanced principle of the amount of water used at the same time, and can exploiting amount predict to groundwater, district of sand,

    本文以寧夏半乾旱地區鹽池縣沙地水資源為研究對象，對該地區多年降水資料、蒸發資料、徑流資料、水文氣象資料、水文地質資料進行了詳盡的分析，分析了沙區的水資源狀況，從地表熱量平衡、水量平衡的基本理論出發，結合沙區的氣象、水文、土壤等資料建立了區域水資源量估算模型，計算了該地區的地表水、地下水，根據實際資料進行了模型檢驗，並對未來不同氣候變化情景下的水資源狀況進行了預測分析，提出了該地區水資源合理利用的方案，運用非線性動力模型對降水量進行預測，同時利用實際觀測資料，運用水量平衡原理計算出沙地地下水的天然補給量，並對沙區地下水可開采量進行預測。
  12. On the regional karst water, it has been primarily clarified that the distributing trait, the cause of formation, and the environment background, and it has been confirmed that the source, the height, and the location about the karst groundwater replenishment. we have found out the relationship of developing circulation among the atmospheric water, the surface water, and the groundwater in the research area, and have compartmentalized the different geohydrology structures about the karst water. 2

    初步查明了研究區的巖溶水分佈特點、巖溶水的成因及形成的環境背景，確定巖溶地下水的補給源區、補給高度、位置及巖溶區內大氣降水，地表水、地下水的動態循環關系，劃分出巖溶水不同的水文地質單元； 2
  13. 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:降水入滲補給系數與地層相關分析的目的，是為推求山丘區降水入滲補給量.魯中山丘區是由各種不同地層出露組成的山丘區域.在多個水文流域基流分割基礎上，建立流域年均降水入滲補給系數與各種地層出露面積占流域總面積權重間的最佳回歸方程，利用該回歸方程和地層分佈及降水量推算不同地下水流域的降水入滲補給量.在地下水開發利用不高的山丘區，降水入滲補給量即為地下水補給量
  14. 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

    由聚類圖推測：祁連山冰川融水通過地下首先經過諾爾圖，然後到達古日乃和拐子湖；古日乃和拐子湖地下水某些樣品聚合距離大，可能是由黑河水滲入引起的，少量黑河水可通過古日乃滲入拐子湖引起地下水成分變化；沒有跡象顯示黑河水補給巴丹吉林沙漠（以諾爾圖為代表）地下水。
  15. In recent years, many barrages have been founded in dagu river, which greatly change the conditions of the exploitation and supply of groundwater. on the basis of calibration of mathematical model of hydrogeology, the effect of diversified factors on the variation of groundwater is analyzed using visual modflow software, the recharge capacity of rubber dam to the groundwater storage is studied and the allowable withdrawl of groundwater with the influence of manpower is calculated again

    近年來大沽河幹流及支流已增加多處攔河壩工程致使地下水采補條件發生了較大變化，本文利用visualmodflow軟體分析了各種影響因素對地下水動態的影響，研究了橡膠壩對地下水庫的補給能力並重新核算了人工影響條件下大沽河地下水庫的允許開采量。
  16. An active measure for ground subsidence control is to move the exploited horizon upward to shallow area and make it close to the recharge and discharge area of groundwater

    控制地面沉降的一個積極措施是將開采層位上移至淺層，使其接近地下水的補給區和排泄區。
  17. More and more people have been aware of groundwater quality change under the long - term utilization of chemical fertilizer in the recharge process

    摘要地下水在補給過程中受到長期施用化肥影響而引起水質的變化已越來越受到人們的重視。
  18. On the basis of examination chapter 6 puts forward the implementary project of utilizing rainwater to recharge groundwater after soil depurating contamination, which exampled by a living zone in xi ' an, and analyses its economic benefits

    第六章在試驗基礎上，以西安市某生活小區為例提出利用城市雨水經土壤層凈化後人工補給地下水的實施方案。
  19. Therefore, cortroling contamination in rainwater is a hot potato in technology of manual recharge groundwater

    因此，雨水中污染物的控制是利用雨水人工補給地下水技術中最棘手的問題。
  20. In dry areas, groundwater completely originate inversion, water cycle and evolution pattern research of groundwater is becoming inversion research of three water, only when we master inversion pattern of water resources, we can evaluate water resources exactly ; ignorance of inversion relationship and unilaterally evaluating water resources must lead to wrong evaluation result

    在乾旱地區，地下水資源完全來自轉化補給，地下水循環與演化規律的研究即成為三水轉化研究的重點，只有準確掌握水資源轉化規律，才能作到準確的水資源評價：忽視資源轉化關系、片面評價水資源必然會導致評價結果失真。
分享友人
分享到 Line

分享到臉書