塔里木河流域水资源变化的特点与趋势

The Tarim RiverBasin islocated in NorthwestChina,which is known in the world forits rich natural resources and fragile eco-environment.W ater resource rational distribution and highly effective utilization isthe key pointsto solve the severe eco-environm …     

塔里木河流域水资源变化的特点与趋势

通过时间序列分析了塔里木河流域山区1961~2002年的降水和温度变化, 源流干流水分的消耗, 并对这些指标进行了KENDALL秩次相关检验。结果显示: 塔里木河源流山区降水和温度均有增加,但是降水增加的趋势在?琢 = 0.05水平上不显著, 温度升高的趋势显著; 塔里木河流域几个源流水量增加, 特别是在1994~2002年,年平均径流量比多年平均增加了25.163×10⁸ m³/a, 而上游三源流补给干流水量只增加0.9985×10⁸ m³/a, 塔里木河干流沿程各站的径流量呈现显著的线性递减趋势, 表明连续十年的丰水期并没有改变干流生态环境恶化的局面; 如果三源流来水以正常年份计算 (1957~2003年平均来水量), 塔里木河干流来水量每年只有22.57×10⁸ m³, 那样塔里木河流域的生态安全将更令人担忧。     

塔里木河流域水资源研究进展

塔里木河是我国最大的内陆河,也是南疆各族人民的母亲河,对其水资源研究的脉络梳理有助于指导当前和未来一段历史时期的水资源研究方向,为水资源合理优化配置提供理论依据,促进南疆经济发展与社会稳定。针对塔里木河流域水资源问题的研究从时间脉络上大致可划分为三个阶段。20世纪50年代之前,主要是中国的历史典籍、自然地理图志和近代国外探险家的探险历程,如实记录了塔里木河的水系变迁和自然风貌,间接反映了流域水资源受到自然-人类活动影响的缓慢变化;20世纪50年代-90年代,随着南疆大规模开发,水资源研究逐渐聚焦于水资源的合理配置与有效管理,其主要针对的是近几十年来人类活动加剧造成的流域内水资源短缺、生态恶化、水资源管理混乱等一系列相关问题;21世纪以来,由于气候变化和人类活动影响造成的塔里木河水文过程变化、水资源承载力及供需矛盾、地下水资源利用与保护等逐渐成为塔里木河水资源研究的新热点。本文在系统梳理三个阶段的研究成果后,进一步提出了未来塔里木河流域水资源研究应的重点关注方向,包括生态调度、水权配置与生态补偿、跨流域调水等。     

塔里木河流域绿洲城镇发展与水土资源效益分析(英文)

This paper examines the spatial pattern of land and water resources as well as urbanization and their interactions in the Tarim River Basin, Xinjiang, China. In order to do so, we extract the data associated with efficiency of land and water resources and urbanization for the years of 1995, 2000, 2005 and 2008. Specifically the paper investigates the extent to which agglomeration of population and economic activities varies geographically and interplays with spatial pattern of resources efficiency through computation of Global Moran’s I index, Getis-Ord Gi* index and a coordinated development model. The method used provides clear evidence that urbanization, land and water resources efficiency have shown uneven spatial pattern due to oasis distribution, climate, and initial phase of urban development. Some conclusions can be drawn as follows.(1) Agglomeration and dispersion of urbanization are not consistent with those of land and water resources efficiency.(2) Evolution of the hot and cold spots of urbanization, and land and water resources efficiency, in different trajectories, indicate that there are no significant interactions between them.(3) The evidence that numbers of hot and cold spots of the three factors present varying structures reveals the dominance of unequal urban development in the study area.(4) Significant differences are also found between sub-river basins in terms of the three factors, which is a reflection of the complex physical geography of the area.(5) The degree of coordinated development of cities in the Tarim River Basin is generally low in part as a reflection of difference in spatial patterns of the three factors. It is also shown that the pattern of the degree of coordinated development is relatively stable compared with evolution of hot and cold spots of the three factors.     

塔里木河三源流区气候变化对径流量的影响

结合对近50年塔里木河源流区气象、水文资料的分析,探讨了过去半个世纪塔里木河源流区气候变化及其对河川径流的影响。研究结果显示,在过去50年里,塔里木河三源流径流流量总体呈现增加的趋势,期间有波动过程;对影响径流变化的气温、降水和蒸发等因子分析发现,降水量变化对塔里木河径流量变化影响最为显著,而温度的升高,加速了山区冰雪资源的消融,加大了冰雪融水对径流量的补给,但同时导致蒸发量增大,增加了地表淡水资源的消耗,对山区来水量的增大起到一定的削弱作用。     

塔里木河流域城市化与水资源利用关系分析

比较分析塔里木河流域1990—2005年城市化水平、用水总量、产业结构、用水效益的变化过程,建立城市化水平与用水效益、用水总量之间的数学关系。结果表明,城市化水平与用水效益呈线性增长关系,随着城市化进程的推进和产业结构的升级,塔里木河流域及各市用水效益都在不断提高;水资源对城市化进程存在明显的约束作用,塔里木河流域的城市化水平与用水总量之间对数增长关系不明显;总结归纳了塔里木河流域城市发展与水资源利用之间初级矛盾、扩张矛盾、适应矛盾、适应协调4个发展阶段特征。今后需调整产业结构,建立集约的水资源利用体系,调整水资源利用与城市发展关系由矛盾状态为适应协调状态,缓解水资源对城市化进程的约束。     

塔里木河流域冰川变化及其对水资源影响

在近一个世纪以来全球变暖趋势显著的背景下,1980年代中后期以来新疆等地区的降水、出山径流出现持续增加现象,冰川也呈加速萎缩状态。作者从区域冰川研究入手,研究在这种气候暖湿转变背景下,塔里木河流域冰川变化的响应及其影响。通过应用大比例尺地形图、高分辨率卫星遥感影像及航空摄影照片获得了塔里木河流域3000多条冰川1960年代初以来的变化,表明该流域近30多年来冰川呈总体萎缩状态,冰川退缩已给塔里木河流域水资源变化带来了明显的影响。     

塔里木河流域水资源分析系统开发研究

根据水资源评价工作的基本任务和实际需求,充分利用计算机及地理信息系统技术,研究和探讨了塔里木河流域水资源分析系统(T-WRAS)的功能、结构、数据组织及其实现关键技术。同时介绍了降水量—高程量化模型(PEM)、自调节水量模拟模型(SRWQ)、基于“发展综合指标测度”的协调程度量化方法(DD)等一些模型和方法。该系统可对三源流汇流过程进行分析,对研究区进行数量、质量、开发利用及综合评价,评价结果以图、文、表等多种形式表达。系统的框架、建设思路及相关模型的研究有一定的理论和现实意义。     

内流河流域水资源利用对径流年际年内变化影响的分析——以塔里木河流域为例

以塔里木河流域为例 ,探讨了干旱区内流河流域近 40年来 ,由于人口增长、灌溉面积扩大、河流水资源引用程度日益增加等原因所引起的河流径流多年变化及年内变化等水文效应及其变化的原因。     

新疆塔里木河流域水资源承载力评价研究

结合塔里木河2002年自然、社会和经济以及水资源资料,选取了耕地灌溉率、水资源利用率、供水模数、需水模数、人均供水量、生态用水率6个主要因素作为评价因素,应用模糊综合评判模型对塔里木河流域水资源承载能力进行了评价研究。结果表明,流域水资源开发利用已经达到相当规模,在现有经济技术条件下,该地区的水资源承载潜力已相对较小,水资源供需矛盾突出,应由耗水型经济结构向节水型经济结构转变,加强水资源的综合管理,以便科学、合理地利用流域内有限的水资源。     

不同水平年塔里木河流域“四源一干”可承载灌溉面积研究

利用水量平衡原理,基于流域水资源量及水资源利用水平、灌溉定额等资料,计算探讨了塔里木河流域“四源一干”现状水平年（2010年）和规划水平年（2020年、2030年）可承载灌溉面积、不同来水频率下规划年灌溉面积超载和生态水保证情况。结果表明：（1）现状水平年,流域可承载灌溉面积为129.06×10⁴ hm²,除和田河流域外其它区域均超载,超载面积为41.7×10⁴ hm²。（2）2020年,25%来水频率下,除开都-孔雀河流域其他区域均不超载。在50%与75%来水频率下,流域规划灌溉面积超载较大,分别为10.21×10⁴ hm²与28.05×10⁴ hm²,管理部门应对规划方案进行科学论证。75%来水频率下,流域生态水保证率为76%,表明枯水期生态水供应存在压力。（3）2030年,25%来水频率下,除开都-孔雀河流域其他区域均不超载。在50%与75%来水频率下,流域规划灌溉面积超载较大,分别为7.06×10⁴ hm²与24.09×10⁴ hm²。75%来水频率下,流域生态水保证率为81%,表明枯水期生态水供应仍然存在压力。研究结果为流域水资源配置及区域可持续发展提供了重要数据支撑与理论依据。     

"水权塔河"体制绩效与未来愿景

塔里木河流域源流初始水权方案政府批准实施,流域机构的行政级别和行政授权不断加强,流域水法规体系建设不断完善,一个围绕水资源使用权管理,并涉及行政、法规、科学管理的“水权塔河”管理体制业已形成。通过流域水权的层次结构和适时水权的管理运行体系系统分析,客观地评价了“水权塔河”的体制绩效以及存在的问题。并提出了构建“水权链”、“目标责任链”和“生态文化”的未来水资源管理模式的三大愿景。     

新疆水文水资源变化及对区域气候变化的响应

Based on the surface runoff, temperature and precipitation data over the last 50 years from eight representative rivers in Xinjiang, using Mann-Kendall trend and jump detection method, the paper investigated the long-term trend and jump point of time series, the surface runoff, mean annual temperature and annual precipitation. Meanwhile, the paper analyzed the relationship between runoff and temperature and precipitation, and the flood frequency and peak flow. Results showed that climate of all parts of Xinjiang conformably has experienced an increase in temperature and precipitation since the mid-1980s. Northern Xinjiang was the area that changed most significantly followed by southern and eastern Xinjiang. Affected by temperature and precipitation variation, river runoff had changed both inter-annually and intra-annually. The surface runoff of most rivers has increased significantly since the early 1990s, and some of them have even witnessed the earlier spring floods, later summer floods and increasing flood peaks. The variation characteristics were closely related with the replenishment types of rivers. Flood frequency and peak flow increased all over Xinjiang. Climate warming has had an effect on the regional hydrological cycle.     

Hydrology and water resources variation and its response to regional climate change in Xinjiang

Based on the surface runoff, temperature and precipitation data over the last 50 years from eight representative rivers in Xinjiang, using Mann-Kendall trend and jump detection method, the paper investigated the long-term trend and jump point of time series, the surface runoff, mean annual temperature and annual precipitation. Meanwhile, the paper analyzed the relationship between runoff and temperature and precipitation, and the flood frequency and peak flow. Results showed that climate of all parts of Xinjiang conformably has experienced an increase in temperature and precipitation since the mid-1980s. Northern Xinjiang was the area that changed most significantly followed by southern and eastern Xinjiang. Affected by temperature and precipitation variation, river runoff had changed both inter- annually and intra-annually. The surface runoff of most rivers has increased significantly since the early 1990s, and some of them have even witnessed the earlier spring floods, later summer floods and increasing flood peaks. The variation characteristics were closely related with the replenishment types of rivers. Flood frequency and peak flow increased all over Xinjiang. Climate warming has had an effect on the regional hydrological cycle.     

塔里木河的水资源利用与生态保护

分析塔里木河1956~2000年间水资源开发利用过程中的生态与环境问题时发现,进入90年代,塔里木河源流区的山区来水量增加了约10.9 %,但是,源流区补给塔里木河干流的水量却减少了18.83 %。三源流灌区用水量的增加导致塔里木河干流区的来水量不断减少,而塔里木河下游来水量的大幅度减少,则是因塔里木河干流上中游耗水量的增加引起。塔里木河干流自身沿程水量变化对下游水量减少的影响,远大于塔里木河上游三源流来水变化对下游造成的影响;塔里木河下游来水量的锐减,造成下游河道断流321 km,尾闾湖泊干涸,地下水位下降,天然植被衰败,沙漠化过程加剧。     

塔里木河干流水资源分配现状及其利用问题

基于塔里木河干流1957-2017年阿拉尔断面、英巴扎断面、恰拉断面来水量特征,首先初步分析塔里木河干流上、中、下游的耗水特征,并基于干流断流和生态输水时间节点,进一步分析1957-1972年、1973-2000年、2001-2017年上中下游各区间段耗水特征,根据这些历史数据变化,从管理角度判别上中下游较为合理的水量分配策略;其次,重点指出塔里木河干流在明确定位为生态河流背景下,未来水量调配精细化管理面临的主要三大基础性问题：灌区耕地面积不清、生态和农业用水量不清、水文数据存在偏差等,并指出问题产生的原因背景,以及从流域水资源管理体制机制上给出相关解决的建议。明确认识到目前塔里木河干流水资源分配利用存在的问题,是未来解决好流域生态环境的关键,通过这些问题的探讨藉此引起更多理性关注,对未来推动塔里木河流域生态环境改善的精细化管理具有重要意义。     

石羊河流域水资源利用和生态环境保护对策

石羊河流域是我各国西北干旱地区的一个重要流域,由于流域水资源的过度开发利用与不合理配置,造成下游地区植被衰败,沙漠化问题十分突出,流域整治和生态环境保护迫在眉睫。本文通过对石羊河流域水资源利用、地下水位下降、土壤盐渍化、植被衰退和土地沙漠化之间的相互作用关系的分析,提出了保证石羊河流域生态用水以防止生态环境劣变和促进流域生态系统良性循环的水资源管理的具体对策建议。     

Impact of climate change and variability on water resources in Heihe River Basin

Studies indicate that the climate has experienced a dramatic change in the Heihe River Basin with scope of temperature rise reaching 0.5-1.1oC in the 1990s compared to the mean value of the period 1960-1990, precipitation increased 18.5 mm in the 1990s compared to the 1950s, and 6.5 mm in the 1990s compared to the mean value of the period 1960-1990, water resources decreased 2.6×108 m3 in the 1990s compared to the 1950s, and 0.4×108 m3 in the 1990s compared to the mean value of the period 1960-1990. These changes have exerted a greater effect on the local environment and socio-economy, and also made the condition worsening in water resources utilizations in the Heihe Rver Basin.     

塔里木河下游植被生态需水量(英文)

We have appraised the relationships between soil moisture,groundwater depth, and plant species diversity in the lower reaches of the Tarim River in western China,by analyzing field data from 25 monitoring wells across eight study sites and 25 permanent vegetation survey plots.It is noted that groundwater depth,soil moisture and plant species diversity are closely related.It has been proven that the critical phreatic water depth is five meters in the lower reaches of the Tarim River.We acquired the mean phreatic evaporation of different groundwater levels every month by averaging the two results of phreatic evaporation using the Qunk and Averyanov formulas.Based on different vegetation types and acreage with different groundwater depth,the total ecological water demand(EWD)of natural vegetation in 2005 was 2.4×108m 3in the lower reaches of the Tarim River.Analyzing the monthly EWD,we found that the EWD in the growth season(from April to September)is 81%of the year's total EWD.The EWD in May,June and July was 47%of the year's total EWD,which indicates the best time for dispensing artificial water.This research aims at realizing the sustainable development of water resources and provides a scientific basis for water resource management and sound collocation of the Tarim River Basin.     

Ecological water demand of natural vegetation in the lower Tarim River

We have appraised the relationships between soil moisture, groundwater depth, and plant species diversity in the lower reaches of the Tarim River in western China, by analyzing field data from 25 monitoring wells across eight study sites and 25 permanent vegetation survey plots. It is noted that groundwater depth, soil moisture and plant species diversity are closely related. It has been proven that the critical phreatic water depth is five meters in the lower reaches of the Tarim River. We acquired the mean phreatic evaporation of different groundwater levels every month by averaging the two results of phreatic evaporation using the Qunk and Averyanov formulas. Based on different vegetation types and acreage with different groundwater depth, the total ecological water demand (EWD) of natural vegetation in 2005 was 2.4×108 m3 in the lower reaches of the Tarim River. Analyzing the monthly EWD, we found that the EWD in the growth season (from April to September) is 81% of the year’s total EWD. The EWD in May, June and July was 47% of the year’s total EWD, which indicates the best time for dispensing artificial water. This research aims at realizing the sustainable development of water resources and provides a scientific basis for water resource management and sound collocation of the Tarim River Basin.