補給河 的英文怎麼說

中文拼音 [bǔgěihé]
補給河 英文
affluxion
  • 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; ...
  • 河 : 1 （天然的和人工的大水道） river 2 （指銀河系） the milky way system; the galaxy 3 （特指黃河） t...
  • 補給 : supply; provision; fitting out; replenishment; feed; recharge
  1. 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。
  2. Food and war supplies from san francisco to noumea, new caledonia ; nitrate from espiritu santo, guadalcanal, suva, antofagasto ( chile ), canal zone, guantanamo bay ( cuba ), arriving savannah on april 3, 1943

    從舊金山運輸食品和補給品到努美阿（新喀里多尼亞島首都） ；在1942年4月3日從聖埃斯皮里圖島、瓜島、蘇瓦島、智利、運河區、古巴運送硝酸鉀到薩凡納。
  3. Efficient and economical artificial recharge projects can often result from utilizing the bed of the main stream channel.

    有效而且經濟的人工補給措施一般可以利用主河道的河床。
  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. 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。
  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. 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。
  9. By comprehensive analysis of hydrogeology condition, hydrology monitoring and particles tracing tests in the cavity area of benxi, the paper researches on the recharged source and its condition of sub rivers this area

    摘要通過對遼寧本溪水洞區域水文地質條件、水文監測和示蹤試驗等資料的綜合分析，對本溪水洞地下暗河的補給源及補給條件等進行了系統研究。
  10. The problem of water quality fluctuation of huanghe river becomes more and more serious in recent years, which exerts great influence on power plants using water from huanghe rive as their feed water

    摘要黃河水量水質隨季節的變化日益明顯，使黃河水水質波動突出，對內蒙古自治區境內以黃河水為補給水的電廠正常生產造成很大影響。
  11. Normally water resources is affected by human activities and climatic change, but it is affected mainly by climatic change in runoff forming regions located in the high and middle mountainous area in the northwestern china. river runoff in the hexi inland arid region all originates from the qilian mt. area and the change of mountainous runoff resulted from global weather warming up and will bring an important effect to the development of society and economy in the hexi region. so the response on mountainous runoff and its changing trends are analyzed on the basis of the measured data of precipitation, air temperature, and discharges observed from some weather and hydrologic stations in the studied area. the results show that seasonal variation of mountainous runoff in the hexi inland region is mainly affected by the river ' s geographical location and supply source, and the yearly change by precipitation and that in the west of the region by air temperature besides precipitation. there are some obviously regional differences in the influences of climatic change on surface runoff in the hexi inland arid region, that is, rivers runoff in the west of the hexi area have been increasing and rivers in the east part have been decreasing, and the rivers runoff in the central part presented slowly increase trend, such as the heihe river, but it is not quite obvious

    一般情況下，水資源的變化主要受氣候變化和人類活動的影響，但在位於我國西北內陸乾旱地區的中高山地帶，徑流的形成主要受前者的影響.甘肅省的河西內陸乾旱區是該省重要的工農業生產和經濟開發區，這里各項社會和經濟活動與出山徑流的變化都有著十分密切的關系.因此，筆者根據有關水文氣象臺站的降水、氣溫和徑流觀測資料，分析了以黑河、昌馬河、西營河等主要河流為代表的河西內陸區出山徑流的變化特徵與規律.結果表明，河西內陸區出山口徑流的季節變化主要受地理位置和河流補給來源的影響，而年際變幅則受山區降水量年際變化及變幅的影響十分明顯.目前，梨園河以西河流水量處于上升階段，梨園河以東的河流則處于下降的階段;以黑河幹流鶯落峽水文站年徑流為代表的走廊中部地區的出山口徑流正處於1990年開始的枯水段的上升段.但總體而言，河西內陸乾旱區出山口徑流的變化相對比較穩定.預計今後若干年內，河西內陸乾旱區東段河流出山口徑流的變化以偏枯為主，中段、西段河流出山口徑流的變化以平水或平水偏豐為主
  12. One exception is tu - wei - he catchment where underground runoff is the primary part of river flow. its runoff season distribution is much uniformity. its runoff amount of july to august accounts is 24 % of the annual runoff amount

    但以地下徑流補給為主的禿尾河，徑流量的季節分配相對均勻， 7 8月份徑流量占年徑流量的24 。
  13. By analysis them, the authors can draw conclusions : the region has horizontal distribution of cretaceous groundwater hydrogeochemistry from east and north and southwest to center

    馬蓮河基流水質的沿途變化規律反映出其接受東西兩側地下水的補給。
  14. 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。
  15. 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 。
  16. 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。
  17. Calculation and analysis of infiltration replenishment in river course

    河道滲漏補給量的計算與分析
  18. 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。
  19. Yellow river replenish to shallow layer ground water system from side. this system is regional shallow layer ground water of hydrological cycle and this system is one of subsystem which belong to groundwater system of north china yellow river flood plain

    黃河水側滲補給淺層地下水系統，是水文循環中一個局部性的淺層地下水系統，是屬華北黃河沖積平原地下水系統的一個子系統，包括黃河水系統和由它演化形成的地下水系統兩個部分。
  20. The study on variation rules of surface water resource indicates the decreasing of rainfall and the increasing of the seasonal snow melting that supply to the yellow river

    研究了青海省地表水資源的變化規律，黃河流域雨水對黃河流量的補給在減少而季節性積雪融水對流量的補給在增加。
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