給水補給 的英文怎麼說

中文拼音 [gěishuǐbǔgěi]
給水補給 英文
feed 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; ...
  • 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 : Ⅰ動詞1 （修理; 修補） repair; mend; patch 2 （補充; 補足;填補） fill up; add supplement; supply; ...
  • 給水 : [機械工程] feedwater; water supply給水泵 feed pump; 給水量 confluent; 給水能力 capacity of water ...
  • 補給 : supply; provision; fitting out; replenishment; feed; recharge
  1. The aquifer is unconfined locally and may be recharged.

    含水層因為局部不承壓而得到補給。
  2. If we give them water and this single - celled algae, we can supply the nutrition

    給他們水和這種單細胞藻類，補給營養。
  3. The phreatic groundwater in the diluvial fan in front of the helan mountain is mainly recharged by precipitation and the lateral flow from the helan mountain ; the phreatic groundwater both in the diluvial fan of the qingtongxia gorge and in the fluvial plain is mainly recharged by the influent seepage of irrigation water from the yellow river

    賀蘭山洪積扇單一潛水主要接受山區側向徑流及大氣降水補給；青銅峽洪積扇單一潛水及沖湖積平原上覆潛水，主要接受黃河灌溉水的入滲補給。
  4. 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。
  5. 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。
  6. Using isotopic ( d, 18o 14c ) geochemical methods, this paper has studied the genetic relationship between the isotopic composition of meteoric water and that of underground hot water, analyzed the supply source of the kaifeng geothermal field and the generation of the geothermal water, and calculated its formation age

    摘要應用同位素（ d 、 18o 、 14c ）地球化學方法，研究大氣降水和地下熱水中同位素組成之間成因關系，分析開封地熱田中地熱水補給來源方向和地熱水的形成，計算其生成年齡。
  7. 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。
  8. Calculating supply amount of karst underground water in spring valley by synthetic permeance coefficieint method is introduced. the question of error in observing all area balanced calculation in fengfeng mine area is expouned

    應用綜合滲入系數法進行泉域巖溶地下水補給計算，解決了峰峰礦區用小流域觀測全區均衡計算過程中誤差較大的問題。
  9. Through the analysis of factors relating to aquiferous features, contact with water, groundwater recharge, run - off, discharge and groundwater chemical characteristics, we determine the hydrogeological conditions in the no. 1 mine field and suggest a basis for deposit exploition

    摘要通過對大南湖煤田一田含水層特徵、水力聯系、地下水補給、徑流與排泄及地下水化學特徵等因素的分析，確定該井田水文地質條件類型，為礦床開采提供依據。
  10. And the more complex the water quality is and the higher the tds is toward the center of basin ; the change of water quality in the malian river indicate that groundwater of the east and west side recharges the river

    說明鄂爾多斯盆地南區的東部地區和西南部地區為地下水補給區，而中心地帶為地下水排泄區，最終經馬蓮河排出區外。
  11. It is concluded that the chemical constituents cluster of glacier melt water in the qilian mountain is the highest one in the region, and the glacier melt water is the main groundwater replenishment source

    計算結果表明，祁連山冰川融水自身化學成分在該地區聚類最高，多次聚合說明祁連山冰川融水是該地區地下水補給源。
  12. Practical application and development of surface and underground water sources recharged with reclaimed water

    國內外再生水補給水源的實際應用與進展
  13. 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

    巖溶水補給來源主要為大氣降水滲入和河流滲漏，排泄方式主要為人工開采和泉水排泄，總體向北徑流，泉域多年平均補給量為55萬m ~ 3 d 。
  14. Using the calibrated model, the effect of diversified factors in the variation of groundwater is analyzed. the result shows that, the change of groundwater level has close relation with the rainfall. in the meanwhile, with the built of rubber dam, it is also been one of an important supply source of the groundwater storage

    模擬結果表明，地下水位的變化與當地降雨量的大小及時程分配，地下水開采量的大小及時程分配和河流來水情況密切相關，其中，降雨入滲、河流滲漏對地下水補給起到決定性作用，同時，隨著橡膠壩的修建，也使其成為地下水庫的一個重要補給來源。
  15. The factors are follows : climate, geology, landforms, hydrology, soil, vegetation, human culture and other factors. compounding the main function, underground water of intake function, in the study area, we can conclude that as thejinan underground water of intake region, the development direction of the study area is to make good use the ecology function, conserve water, maintain water and soil, modulate culture, clean air, improve water quality, beautify environment

    （ 2 ）分析研究區景觀生態系統要素：氣候、地質、地貌、水文、土壤、植被、人文等要素，結合研究區主要生態功能，地下水補給功能，分析人類活動對研究區景觀結構功能的影響，得出研究區生態環境質量較差，破壞嚴重，不利於物質、能量流動，與其所要求景觀功能不相適應，現已成為區內經濟發展的主要限制因素。
  16. On the foundation of reference researches, through analyzing the condition of rainfall and hydrogeology of tian - tang river in the suburb of south - east of beijing, the mathematical models of the shallow ground water movement were founded. according to the experiment result of pump water and other reference data, the parameter of hydrogeology and ground water were established. on the foundation of present and future trend of using water on industry, agriculture and living, the solution of mathematical models were calculated by the method of finite element

    在前人研究的基礎上，本文通過對北京市東南郊天堂河流域降雨、水文地質條件的分析，建立淺層地下水運動數學模型，根據抽水試驗結果並參考有關資料確定水文地質和地下水補給的有關參數，根據工業、農業、生活現狀用水情況及未來的發展趨勢，採用有限元的方法對地下水運動數學模型進行求解。
  17. ( 2 ) because of t he variability of rock subjected to outside action, three new conceptions : postive damage basic damage and negative damage, are suggested, which can deal with the condition that rock density became large. ( 3 ) the present damage variables based on ct number mostly include ct average number of the rock without damage, which is difficult to measure, so a new damage variable, which includes the average ct number is proposed, on the other hand, strain equal theory is generalized because the one put foreword by lemaitre is not good enough to use. ( 4 ) a axial damage constitutive equation is proposed and testified. ( 5 ) with the circle times, the damage propagation laws of two different rocks, subjected to circle of freezing and thawing, are studied, and in the analysis process, traditional analysis method including average ct number and is used, some important conclusions are reached : inner damage of soft rock containing a large mount of apertures is largely propagating with the time increasement of circle, however, at the preliminary time, the hard rock containing a small mount of aperture is a little propagating, at late time, the influence become large ; ( 6 ) zone separation and statistics frequency put forward is used to analysized the three different damage propagation in the open circumstance, when they are subjected to the different circle times of freezing and thawing, in which the temperature variability is linear, different freezing rate, and different freezing temperature, and no water is supplied during the test

    在研究過程中本文主要做了以下工作： （ 1 ）針對巖石損傷變化較小時，運用ct均值和方差分析不方便的缺陷，本文提出運用對ct數范圍劃分區段的方法，根據各區段統計頻率的變化規律來分析損傷擴展狀況； （ 2 ）針對巖石受到外部作用的多變性，本文提出了基準損傷，正損傷，負損傷的概念，在某種程度上考慮了巖石受到外部作用時的壓密情況； （ 3 ）現有的基於ct數的損傷變量大多需要用到巖石基體的ct均值，這實際上是很難觀測到的，因此本文建議了一個可運用巖石初始狀態ct均值的損傷變量，由於現有的勒邁特教授應變等價原理使用上的不便，本文在其基礎上進行了推廣； （ 4 ）建議了一個可用巖石初始狀態ct數和彈性模量的單軸損傷本構方程，並用算例進行了驗證； （ 5 ）對兩種不同巖石在開放環境下受到凍融循環作用且融化過程中補水時，內部損傷隨凍融循環次數增加的擴展規律進行了探討，主要運用了常規的ct均值和ct方差的分析方法進行分析，試驗發現：對于孔隙率和含水率較高，密度和強度較低的軟弱巖石，凍融循環次數對損傷結構的擴展有明顯的影響，而對于孔隙率和含水率較低，密度和強度較高的硬巖，凍融循環次數對其損傷結構擴展初期由於含水率低的原因，影響不是太大，而後期由於水補給后，含水率較高的原因，凍融影響逐漸增大； （ 6 ）運用了本文提出的區段劃分和統計頻率的方法，深入地分析了開放環境下的線性溫度變化的凍融循環次數，凍結溫度，凍結速度不同巖石作用時，其內部損傷隨凍融循環次數，凍結速度和凍結溫度變化的擴展規律，需要指出的是除了在試驗前飽水外，凍融過程中沒有補水。
  18. That could produce floods and reduce water supplies over time

    隨著時間的推移，這種趨勢很可能導致洪水泛濫，水補給下降。
  19. In the term of principles of regional conservational development, to define the area in which we can have estate objection, where concentrate in the area of beikang, nankang, jiuqu and from yuanbaishan to shaoer whose surface area is 5. 0 km % ( 4 ) in the light of ground water recharge function, the main way to define contents including existing green conservation, water source region conservation is to ecology construct

    按照區域保護性開發的原則，界定可適宜進行房地產開發的建設區域，主要集中在北康、南康、九曲及元白山至邵而莊一帶，面積約5 . 0km ~ 2 。 （ 4 ）根據研究區的主要生態功能：地下水補給功能，研究區內保護重點為現有綠地的保護、水源地的保護。
  20. The geothermal water can be classified into three categories based on the time when replenishment take place and mixing extent with normal groundwater which are : geothermal water mixing with normal groundwater recharged mainly by the modem meteoric water ; geothermal water mixing with normal groundwater water recharged by both ancient and modem meteoric water ; deep - runoff geothermal water recharged mainly by ancient meteoric water

    根據降水補給的年代及混合程度可將地下熱水分為主要由現代大氣降水補給的混合型地下熱水；由現代大氣降水和古代降水補給的混合型地下熱水；主要由古代大氣降水補給的深部循環型地下熱水。
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