upper reaches of tarim river 的翻譯結(jié)果
本文關(guān)鍵詞:干旱區(qū)綠洲農(nóng)業(yè)生態(tài)經(jīng)濟(jì)系統(tǒng)的結(jié)構(gòu)和功能分析——以塔里木河上游的阿克蘇地區(qū)為例,由筆耕文化傳播整理發(fā)布。
在分類(lèi)學(xué)科中查詢(xún) 所有學(xué)科 環(huán)境科學(xué)與資源利用 自然地理學(xué)和測(cè)繪學(xué) 農(nóng)業(yè)經(jīng)濟(jì) 歷史查詢(xún)
upper reaches of tarim river
Analysis on the Utilization Efficiency of Water Resources in the Upper Reaches of Tarim River, Xinjiang
塔里木河上游水資源利用效率分析
短句來(lái)源
Structure and Function of Agriculture Eco-economy System in Arid Area Oasis——Take Aksu Area at Upper Reaches of Tarim River for Example
干旱區(qū)綠洲農(nóng)業(yè)生態(tài)經(jīng)濟(jì)系統(tǒng)的結(jié)構(gòu)和功能分析——以塔里木河上游的阿克蘇地區(qū)為例
短句來(lái)源
Profit and loss analysis on ecological value in upper reaches of Tarim River under land use changes
塔里木河上游土地利用變化中的生態(tài)價(jià)值損益分析
短句來(lái)源
Based on the TM images of 1990 and 2000,this paper analyzed the land use changes in Akesu-Awati oasis at the upper reaches of Tarim River,and,with the equivalent weight factors of ecosystem services,estimated the ecological value under these changes.
利用1990和2000年2期TM影像,對(duì)塔里木河上游典型綠洲的土地利用面積變化進(jìn)行了研究,在土地利用變化背景下,通過(guò)貨幣化生態(tài)服務(wù)功能,揭示塔里木河上游典型綠洲生態(tài)價(jià)值的變化。
短句來(lái)源
Analysis on Landscape Change and Estimation on the Ecological Valuation of Typical Oasis in the Upper Reaches of Tarim River
塔里木河上游典型綠洲景觀變化分析及其生態(tài)價(jià)值損益估算
短句來(lái)源
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The Dynamics of Land Utilization inthe Upper reaches of Tarim River
塔里木河干流上游土地利用動(dòng)態(tài)變化研究
短句來(lái)源
On the Upper Reaches of Money Laundering
論洗錢(qián)罪之上游犯罪
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On Industrialization of Farming in the Upper Reaches of the Yangtze River
論長(zhǎng)江上游地區(qū)農(nóng)業(yè)產(chǎn)業(yè)化
短句來(lái)源
the type of supplier seeking profit from the upper reaches;
從上游供應(yīng)商尋求利潤(rùn)型;
短句來(lái)源
Prevention Countermeasures in the Upper Reaches of Min River
岷江上游生態(tài)環(huán)境治理對(duì)策探討
短句來(lái)源
Population characteristics in upper reaches of Minjiang River
岷江上游人口特征
短句來(lái)源
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The regularities of water transform in stream forming area and disappearing area are quite different. In stream forming area, water transform is mainly that groundwater flows out to form surface water. And in stream loss area, water transform is mainly that surface water seeps into ground. At the perimountain plain, when the transform of surface water-groundwater- surface water finishes, it may begin the second transform if there is a structural basin in the lower reaches of rivers. However, water...
The regularities of water transform in stream forming area and disappearing area are quite different. In stream forming area, water transform is mainly that groundwater flows out to form surface water. And in stream loss area, water transform is mainly that surface water seeps into ground. At the perimountain plain, when the transform of surface water-groundwater- surface water finishes, it may begin the second transform if there is a structural basin in the lower reaches of rivers. However, water becomes less and less after the process of transform. Effect of water to environment can be divided into two types, natural effect and human effect. The changes of natural conditions need a long time of geological period. The influences of human activities take place in a short time and regionally, especially in arid land where water is the key factor of environment. Hydrological changes in Xinjiang are mainly that: part of river courses has been replaced by artificial canal system; some lakes are replaced by reservoirs; and water table has changed. Located at the upper reaches of Tarim River, Afar irrigation area is reclaimed after 1958. With the expansion of irrigation area after land reclaiming, much of water seeped into ground from canals and farmland to feed groundwater. Seasonal change of water table is based on irrigation periods. Mineralization of groundwater has reduced but most of the drained water flows into rivers or lakes, river water quality has changed too. The redistribution of water is mainly that: water quantity has been improved within oases, but runoff in the lower reaches has reduced. Alar irrigation area is the largest new oasis with stable agricultural eec-environment in Tarim Basin since the redistribution of water resources. Hydrological and climatic conditions are improved within the oasis.
新疆的水平衡特征是,徑流形成于山區(qū),流到平原區(qū)后不斷蒸發(fā)和滲漏,最終消耗在沙漠中,,或者流入尾閭湖。由于人類(lèi)活動(dòng)的影響,水的分布和轉(zhuǎn)化都發(fā)生了改變,綠洲中的水量增加,但綠洲以外與河流下游的水量減少,同時(shí)有些湖泊縮小甚至干涸,沙漠化發(fā)展,自然植被衰退,自然環(huán)境退化。
Most of the groundwater in mountain area is transferred to ground surface as the runoff in Xinjiang.Groundwater at plain area mainly comes from infiltration of river water,lakes,canal system,reservoirs and irrigation.And 78.5% of it is seeped river water.Infiltrating water in agricultural area is caused by human activities,which has changed the water table and groundwater quality to a great extent,and changed the movement process of groundwater. \ \ Alar irrigation area established in 1958 located...
Most of the groundwater in mountain area is transferred to ground surface as the runoff in Xinjiang.Groundwater at plain area mainly comes from infiltration of river water,lakes,canal system,reservoirs and irrigation.And 78.5% of it is seeped river water.Infiltrating water in agricultural area is caused by human activities,which has changed the water table and groundwater quality to a great extent,and changed the movement process of groundwater. \ \ Alar irrigation area established in 1958 located in the upper reaches of Tarim River.It has increased the quantity of water within the area and caused the rise of groundwater to draw water from river for irrigation.Irrigation and drain water away to wash salt in the soil have improved groundwater quality in the oasis,but the surface water in Tarim River has mineralized because it takes up salt water drained from farmland.Not only the water table in oasis had gone up,but also it varies obviously in different seasons.It is 1.5 ̄2.0m higher in summer than in winter,and it would rise for 0.2 ̄0.5m after each irrigation. \ \ The decline of water table out of oasis has caused the decrease of soil moisture so that the ground surface is quite dry and part of the natural vegetation has died,and the weather with floating dust has increased after 1980. \ \
本文分析了新疆地下水的轉(zhuǎn)化規(guī)律,特別是平原區(qū)地下水的補(bǔ)給關(guān)系。對(duì)塔里木盆地阿拉爾地區(qū)開(kāi)墾后的地下水變化特征和人類(lèi)活動(dòng)對(duì)地下水的影響做了重點(diǎn)分析。結(jié)果表明人類(lèi)活動(dòng)改變了水資源的分布狀況,使綠洲內(nèi)部地下水位上升,水質(zhì)改善;但綠洲以外地下水位下降,河流由于接納了綠洲排水,水質(zhì)變差。
Water resources are becoming more and more shortage in Tarim arid region. So it is important to control the expansion of land reclamation and enhance the efficency of water resources utilization in upper reaches of Tarim River. It is also significant for the development of Tarim region to resolve the conflict between agricultural using water and ecological using water. Remote sensing technology is the best way to analyze the dynamics of land use. In this paper, the author discussed the dynamics...
Water resources are becoming more and more shortage in Tarim arid region. So it is important to control the expansion of land reclamation and enhance the efficency of water resources utilization in upper reaches of Tarim River. It is also significant for the development of Tarim region to resolve the conflict between agricultural using water and ecological using water. Remote sensing technology is the best way to analyze the dynamics of land use. In this paper, the author discussed the dynamics of land use in typical region-Alaer(K-44-127,1∶100,000) by using the aeronautical maps and satellitic maps which were made in 1959,1983,1992 and 1996. The results showed that in this region the artificial oasis and residential area were enlarged step by step. On the contrary, the area of natural vegetation shrank year by year. As for the other land using types, the area of lakes decreased quickly and the area of usless land types has no great change for these years, e.g. the desert and the salina. Therefor the local goverment should strictly control the enlargement of land reclamation in upriver of Tarim River in order to save the lower reaches of Tarim River. And at the same time, we should strengthen the construction of vegetation to improve the ecological environment.
在干旱區(qū) ,水資源十分匱乏。若能有效的控制塔里木河上游耕地面積的擴(kuò)張 ,同時(shí)提高水資源利用率 ,則能解決塔里木河流域長(zhǎng)期以來(lái)農(nóng)業(yè)用水和生態(tài)用水之間的矛盾 ,這對(duì)塔里木河流域持續(xù)發(fā)展有重要意義。應(yīng)用遙感技術(shù)進(jìn)行上游土地利用動(dòng)態(tài)變化則為上游耕地現(xiàn)狀和趨勢(shì)發(fā)展提供一種快速和準(zhǔn)確的方法。本文利用 1 95 9年、1 983年、1 992年和 1 996年四個(gè)時(shí)期的航片及衛(wèi)片資料 ,研究了塔里木河干流上游典型圖幅土地利用的動(dòng)態(tài)變化。結(jié)果表明 ,研究區(qū)域人工綠洲和居民點(diǎn)面積逐年擴(kuò)大 ,湖泊面積明顯縮小 ,而天然植被面積趨于縮小 ,難利用面積變化不大。為此 ,有關(guān)部門(mén)應(yīng)嚴(yán)格控制目前這種耕地繼續(xù)擴(kuò)張趨勢(shì) ,同時(shí)加強(qiáng)植被生態(tài)環(huán)境建設(shè)
 
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本文關(guān)鍵詞:干旱區(qū)綠洲農(nóng)業(yè)生態(tài)經(jīng)濟(jì)系統(tǒng)的結(jié)構(gòu)和功能分析——以塔里木河上游的阿克蘇地區(qū)為例,由筆耕文化傳播整理發(fā)布。
本文編號(hào):210025
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