1) upper reaches of Tarim River
塔里木河上游
1.
euphratica forest of Awati county in upper reaches of Tarim River,sampling by contiguous grid quadrate method and making use of such indexes as variance/mean ration,negative binomial parameter,diffusing index,cassie index,clumping index and patchiness index.
以新疆塔里木河上游阿瓦提县天然胡杨林为研究对象,采用相邻格子法进行实地调查,应用方差/均值比率法和5种聚集度指标研究了塔里木河上游天然胡杨林主要种群的空间分布格局与动态特征。
2) lower reaches of the Tarim River
塔里木河下游
1.
Arbuscular mycorrhizaes of common plants infection at the lower reaches of the Tarim River;
塔里木河下游丛枝菌根植物的侵染
2.
Ecological-economic values of the natural vegetation restoration after groundwater elevation at the lower reaches of the Tarim River;
塔里木河下游地下水抬升的地表植被恢复价值初探
3.
Influence of seed morphology on the vertical distribution of a soil seed bank in the lower reaches of the Tarim River;
塔里木河下游植物繁殖体形态对土壤种子库垂直分布的影响
3) lower reaches of Tarim River
塔里木河下游
1.
Factor analysis in environmental degradation at the lower reaches of Tarim river;
塔里木河下游环境退化的因子分析
2.
Dynamic change of groundwater after ecological water transport at the lower reaches of Tarim River;
生态输水后塔里木河下游地下水的动态变化
3.
Monitor of ecological response along lower reaches of Tarim River based on remote sensing;
塔里木河下游生态响应遥感监测研究
4) middle reaches of Tarim River
塔里木河中游
1.
Research area located in the middle reaches of Tarim River,and land use types in this area include cultivated land,oil-gas field,and water transfer dike etc.
本研究区位于塔里木河中游地区,本研究选取耕地变化、输水堤防的建设以及油气田开发三种土地利用方式,在大量野外调查的基础上,在3S技术和历史数据的支持下,分析了这些土地利用方式变化对胡杨林生态系统的影响。
2.
Yarkandensis)in middle reaches of Tarim River.
2006年7月和12月在塔里木河中游塔里木胡杨林自然保护区对塔里木马鹿夏季和冬季生境的选择进行了研究。
5) The lower reaches of the Tarim River
塔里木河下游
1.
Variation of groundwater level after ecological water transport in the lower reaches of the Tarim River in recent six years;
塔里木河下游断流河道输水后潜水埋深变化规律研究
2.
In the lower reaches of the Tarim River,it belongs to the warm-temperate arid climate,the annual solar radiation,sunshine duration,accumulated temperature ≥10 ℃ and average daily range of temperature vary in ranges of 5 692～6 360 MJ/m~2,2 780～2 980hours,4 040～4 300 ℃ and 13～17 ℃ respectively.
结合2002-2004年对塔里木河下游生态输水过程中5个断面固定植物群落样地的调查,运用群落数量分析法,分析了塔里木河下游植物群落对生态输水的响应。
3.
In this paper, the chemical properties of groundwater are studied during four times of transfusing stream water to the lower reaches of the Tarim River for regenerating the ecology so as to reveal the temporal and spatial response of chemical properties of groundwater to implementing the project of transfusing stream water along the Yengisu section.
通过对塔里木河下游地下水化学特征在 4次生态输水后的变化分析 ,揭示英苏断面地下水矿化度对生态输水的时空响应特点。
6) the lower reaches of Tarim river
塔里木河下游
1.
Effect of Translating Water on Vegetation at the Lower Reaches of Tarim River;
塔里木河下游生态输水对植被和地下水位的影响
2.
The characteristics of the soil seed banks follow different groundwater depth in the lower reaches of Tarim River;
塔里木河下游不同地下水埋深下的土壤种子库特征
3.
The structure characteristic of the plant community in the lower reaches of Tarim River;
塔里木河下游植物群落结构特征分析
补充资料：塔里木河
| 塔里木河 中国第一大内陆河。位于新疆维吾尔自治区塔里木盆地北部。上游有三源：阿克苏河源出天山山脉，叶尔羌河及和田河源出喀喇昆仑山脉，在阿瓦提县肖夹克附近汇合后称塔里木河。在尉犁县以南折向东南，穿过塔克拉玛干沙漠的东北部，注入铁干里克的大西海子水库。若从叶尔羌河上源算起，至大西海子长2000千米，若从阿克苏与叶尔羌河相汇处算起，到大西海子长800千米，流域面积19.8万平方千米。塔里木河在历史上曾多次改道。1921年主流下游北移，东流沿孔雀河注入罗布泊。1952年中段的汊流拉因河口筑起塔里木大坝，阻断河水流入孔雀河，河道主流改沿铁干里克故道，折向东南流入台特马湖。现在，塔里木河仅到铁干里克流入大西海子水库，台特马湖处干涸状态。河水主要来自阿克苏河（占72.0％） 、和田河（占22.5％） 、叶尔羌河（占5.5％） 。上段的阿拉尔站，每年有49亿立方米水量下泄，沿途蒸发与渗漏严重，致使大西海子以下至台特马湖的河段断流，引起大片胡杨树枯死，沟通塔里木盆地南北的绿色走廊面临毁灭的危险。 |
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参考词条