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lakes in xinjiang
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  新疆湖泊
     A Study on the Hydrochemistry of Lakes in Xinjiang
     新疆湖泊水化学研究
短句来源
     The Climate Trend Demonstrated by Changes of the Lakes in XinJiang Since Recent Yesar
     近期新疆湖泊变化所示的气候趋势
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  “lakes in xinjiang”译为未确定词的双语例句
     The Formation and Evolution of the Environment of Salt Lakes in Xinjiang, China
     新疆盐湖的形成演化环境
短句来源
     16S rDNA PCR-RFLP ANALYSIS OF MODERATELY HALOPHILIC BACTERIA ISOLATED FROM SALT LAKES IN XINJIANG REGION
     新疆地区盐湖的中度嗜盐菌的16S rDNA PCR-RFLP分析
短句来源
     SALT MINERALS AND THEIR MECHANISM OF THE SALT LAKES IN XINJIANG
     新疆现代盐湖盐类矿物及有关成盐机制
短句来源
     Research on the hydrochemical feature of the brine of salt lakes in Xinjiang
     新疆盐湖卤水水化学特征研究
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     The Nitrate Salt Lakes in Xinjiang
     新疆的硝酸盐盐湖
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  相似匹配句对
     Wuhan Rivers and Lakes
     江湖武汉
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     Lakes in the Gobi Desert
     太空看中国·戈壁中的湖泊
短句来源
     On Saline Lakes of China
     论中国盐湖
短句来源
     ON THE ARTIFICIAL EUTROPHICATION OF LAKES
     湖泊人为富营养化
短句来源
     Xinjiang is included.
     新疆被划入“天然林保护工程”实施的范围。
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Covering an area of about 400 km2, lake-shore swamps of Bositeng Lake in Xinjiang is the largest .areal swamp land in the arid zone of China. This area is of the to temperate desert climate. Kaidu River with an origin in Tianshan Mountain and other creeks discharge a total of 41.6×108m3 water annually into the Yanqi basin. This stable water supply is the leading factor for swamp formation. Yanqi basin is a good place for swamp formation and peat accumulation. .Swamps in this area are formed by the...

Covering an area of about 400 km2, lake-shore swamps of Bositeng Lake in Xinjiang is the largest .areal swamp land in the arid zone of China. This area is of the to temperate desert climate. Kaidu River with an origin in Tianshan Mountain and other creeks discharge a total of 41.6×108m3 water annually into the Yanqi basin. This stable water supply is the leading factor for swamp formation. Yanqi basin is a good place for swamp formation and peat accumulation. .Swamps in this area are formed by the paludification of waferbody. The swamp is mainly of the eutrophic herb reed and eutrophic herb Typha type in the luxuriantly developing-stage. Swamp is rich in reed and peat resources. The annual production of good quality reed can reach 22.95 ×104t, an abundant raw material resource for papermaking industry. Peat reserves in swamps are nearly 10s t. But peat in this area is unsuitable for large scale exploitation.Bositeng Lake and the lakeshore swamps are the special ecosystem under desert climate conditions, which plays an important role in maintaining regional ecological balance.

新疆博斯腾湖的湖滨沼泽是我国干旱区面积最大的沼泽地。稳定的水源补给是沼泽形成的主要因素,凹陷盆地为沼泽形成和泥炭堆积提供了良好的空间场所。本区沼泽来源于水体沼泽化,沼泽类型比较单一,蕴藏着丰富的芦苇和泥炭资源。博斯腾湖及其沼泽在维持区域生态平衡中具有重要的作用。

Through many synchronous analysis of lacustrine deposit from Hole Zk 0024 in the Balikun Lake in Xinjiang, it is known that, since Holocene, the lake's water level has undergone multiple expansion and contraction periods, corresponding to multiple alternations of cold-humid and hot-dry climates in the lake area. In the meantime, several advancing and retreating processes in glacial and interglacial stages occurred in mountainous region. Water level, palaeoclimate and glacial period all went...

Through many synchronous analysis of lacustrine deposit from Hole Zk 0024 in the Balikun Lake in Xinjiang, it is known that, since Holocene, the lake's water level has undergone multiple expansion and contraction periods, corresponding to multiple alternations of cold-humid and hot-dry climates in the lake area. In the meantime, several advancing and retreating processes in glacial and interglacial stages occurred in mountainous region. Water level, palaeoclimate and glacial period all went through 4 regular synperiodic varia tions, making up a unification in Holocene environmental evolution in the Balikun Lake area.

新疆巴里坤湖ZK0024孔湖相沉积经多种手段同步分析表明自全新世以来,当湖区古气候多次出现不同程度的冷湿与暖干交替变化时,反映巴里坤湖发育史上经历了多次水位扩张期与收缩期的演变过程,此时山区则表现为全新世以来几次冰期与间冰期的进退变化,三者均呈现有规律的同周期变化,构成巴里坤全新世环境演变统一发展的整体。

The plain lakes in Xinjiang have changed a great deal as a result of human's activities. Besides that some of them have become smaller or dried up, water salinzization of the lakes gives rise to a very conspicuous problem either. For example, the water mineralization of the Bosten Lake, the largest interior freshwater lake in China, raised from 0.25-0.40g/l in 1958 to 1.80-1.90g/l in 1986 and this freshwater lake has changed into a saltwater one to a certain extent. The water mineralization...

The plain lakes in Xinjiang have changed a great deal as a result of human's activities. Besides that some of them have become smaller or dried up, water salinzization of the lakes gives rise to a very conspicuous problem either. For example, the water mineralization of the Bosten Lake, the largest interior freshwater lake in China, raised from 0.25-0.40g/l in 1958 to 1.80-1.90g/l in 1986 and this freshwater lake has changed into a saltwater one to a certain extent. The water mineralization of other lakes such as the Buluntuo Lake and the Ailike Lake has increased notably. The water salinization of plain reservoirs is becoming more and more serious from day to day. The water salinization of lakes and reservoirs could exert an unpleasant influence on fishing, irrigation, reed growth, drinking water, and people's health. It is mainly the deterioration of salt balance and water balance that resulted in the water salinization. For the prevention and control of the water salinization, we have to drain less farm fields water into the natural river courses and lakes in order to ensure the water supply for ecologic purpose and put an end to the loss state in which the water balance of lakes has been for a long time.

新疆平原湖泊、平原水库盐化日趋严重。湖泊、水库水质盐化对渔业、灌溉、苇产、饮水和人体健康带来很大影响。引起湖泊、水库水质盐化的原因,主要是人为活动造 水盐与水量平衡关系改变的结果。为防止水质盐化,必须减少农田排水泄入河道和湖泊、增加入湖水量,扭转湖泊水量平衡长期亏损状态。

 
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