補給區 的英文怎麼說
中文拼音 [bǔgěiqū]
補給區
英文
accumulation area-
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。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。Based on analysis of geologic foundation record about pingzhuang basin, a lot of sino - foreign geothermal geology record and investigation of field geology, measuring of ground temperature in person and geo - chemical analysis of ascension spring, gushing water of fault, the fact that the anomaly of geothermal gradient of pingzhuang basin, which is in region of low geothermal gradient, is caused by redistribution of conduction - oriented geothermal heat flow which is result from upheaval and depression of basin foundation bed is pointed out. after the field of ground temperature is simulated under the background of conduction - oriented geothermal heat flow by means of ansys, the characteristic of ground temperature distribution of top surface of basin foundation bed ( yixian team ) is revealed. the sound condition of transmissibility fault and feeding water source, which are imperative in formation of the low - medium temperature geothermal system of convective type, is possessed in pingzhuang basin
通過對平莊盆地基礎地質資料、國內外大量地熱地質資料的分析和野外地質調查、礦井實測地溫以及上升泉、斷層涌水的地球化學分析等工作基礎上，指出地處低地溫梯度背景區的平莊盆地地溫梯度異常是由於盆地基底隆起和坳陷引起傳導型大地熱流再分配所致；運用州sys數值模擬了大地熱流向地表傳導背景下的盆地地溫場，從而揭示了盆地基底（義縣組）頂界面地溫分佈特徵；闡明了盆地具有形成中低溫對流型地熱系統所必需的導水斷裂、補給水源等的良好條件，中低溫對流型地熱系統是地熱勘查的主要對象；圈定了平莊盆地北部朝陽溝?駱駝營子地熱勘查遠景區。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。Afarv armored forward area rearm refuel vehicle
前方地區裝甲彈藥及燃油補給車And supplies from surplus regions in southern sudan
.和對蘇丹南部其他地區的補給( 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。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。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。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； 2Abstract : 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。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。This paper evaluates the underground water resources and its safe levels of miming, and then studies the availability of molepipe drainage, a kind of practical underground water regulation technique. starting with the elevation of underground water resources and a safe level of mining through variable system theory, this paper analyzes the conditions of underground water resources based on the well - studied determination method of determining the two hydrographical coefficients : rainfall infiltration replenishment rate and irrigation replenishment rate. then considering irrigation, rainfall, drainage and other related factors, a mathematical model is set up for the calculation of underground water storage, exploitation on water regulation
論文從灌區的地下水資源及其可開采量評價分析方面入手，在對兩個主要的水文地質參數即降雨入滲補給系數、灌溉入滲補給系數確定方法研究的基礎上，對灌區的地下水資源狀況進行分析，依據灌區的灌溉、降雨、排水條件及各種現狀因素，建立了地下水資源量計算的數學模型，西安理工大學工程碩士專業學位論文計算得到青銅峽灌區地下水的最大補給量和可開采量;另外對在開發利用地下水資源過程中的地下水位的調控進行了初步的探討，在銀北灌區開展對暗管排水調控地下水位的試驗研究。The karst water moves from south to north. after moving to jinan city, the karst water is blocked by igneous bodies, the karst water passes through fissures and karst and gushes out to the surface as springs
來自南部補給區的巖溶地下水徑流至老城區附近，遇到巖漿巖體阻隔，在地形低洼部位通過淺部石灰巖巖溶裂隙湧出地表，形成濟南諸泉。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。Do whole of the groundwater flow from the western recharge area to eastern
地下水是否都從西部補給區向東徑流This article will mainly introduce, analyze endangering characterstices of karst and the investigating methods in recharge area, runoff area, drainage area through engineering examples
本文結合典型工程實例分別介紹了巖溶補給區，徑流區和排泄區的地質危害特點、類型及相應的勘察方法。The fenshuiling - dajiangou - jiuqu region, an important ecological protection area of shandong province, lies in the southward hilly region in jinan. it is a significant ecological function area and one of spring intake regions
分水嶺?大澗溝?九曲地區位於濟南市南部山區，是濟南市重要的生態功能區，濟南市泉域重要補給區之一，為省級重點生態保護區。The author validate that precipitation is the source of juzhai valley by using of isotopic. changhai in the recharge area receives the precipitation and thawing water, which drains along the rupture towards rize valley and jiuzhai valley so changhai has the important effect on the whole area
運用回歸方法得山位於補給區的長海之水來源於大氣降水的冰雪融水，並沿斷裂補給到日則溝和九寨溝，因此長海水量多寡來源直接到本區湖泊水體的穩定。分享友人