开发建设项目水土保持监测与评价——以玛纳斯电厂三期扩建工程为例

对新疆玛纳斯电厂三期扩建工程进行水土保持监测与评价分析.结果表明,在工程施工初期,地表结构受到扰动与破坏,增加了水土流失量.到施工后期(水保方案运行期),随着对土体结构、地表状况和植被的逐渐恢复,人为扰动因素逐渐减少,地表开始逐步恢复,土壤侵蚀量也逐步趋于稳定.在项目区多数地段,工程施工并未引起大面积严重水土流失;项目...     

新疆干旱荒漠生态环境监测站建站拉开序幕

新疆干旱荒漠生态站的前期工作是从1985年开始的,在近五年中,新疆环境监测中心站生态室的同志,结合新疆实际进行了大量的可行性研究。于1988年提出了新疆干旱荒漠生态环境监测站的建站方案。在国家环保局的主持下,对新疆干旱荒漠生态环境监测站建设计划任务书进行了论证,专家们认为:由于不合理开发自然资源,致使生态环境恶化,已引起人们的关注。新疆已存在明显的土地沙化、盐渍化、河水断流、湖泊干枯及绿洲生态系统环境质量下降。开展生态监测能及时了解和掌握生态环境的质量变化状况,为环境保护部门强化管理和合利利用自然资源提供科学依据,具有战略意义。国家环保局在     

新疆土地生态环境问题与对策

土地生态环境是人类生存发展的基本条件,是经济、社会发展的基础.在当前的经济形势下,包括水土流失、土壤盐碱化、植被破坏等一系列土地荒漠化问题以及由于荒漠化而造成的生物多样性受损引起人们的广泛关注.为了实现经济的可持续发展目标,加强新疆的综合竞争能力,在区域开发过程中要注重土地生态环境建设.本文对新疆土地生态环境现状与存在的问题进行分析,阐明了土地生态环境恶化的原因,提出土地生态环境建设的对策.     

准噶尔盆地西北部引水工程建设运行的生态环境效益评估

准噶尔盆地西北部引水工程的建成和运行,对工程沿线区域土地资源的利用方式产生了深远的影响,也改变了该区域以土地资源为载体的生态系统的结构和生态环境的价值。以Constanza等人对全球各类生态系统单位面积服务价值的测算为依据,根据准噶尔盆地西北部引水工程沿线影响区2000年和2002年LandsatTM卫星影像解译数据,对工程建设和运行的生态环境效益予以估算。结果表明:引水工程的建设运行使工程影响区内生态系统的生态环境效益增加了2657 14×104 (约合22054 26×104元人民币),其中水域及耕地生态系统生态效益的增加是研究区生态效益增加的主要方面。     

新疆环境监测中心站积极开展生态环境遥感监测工作

新疆独特的地理环境造就了区域典型的大陆性干旱气候 ,加之人类不合理的开发 ,使新疆生态环境极其脆弱。为了及时准确地掌握和了解新疆宏观生态环境的现状 ,自治区环境监测中心站积极开展生态环境遥感监测工作。监测技术人员在获取全区气象卫星 NOAA— 12五个波段影像数据的基础上 ,利用遥感软件完成了全区和有关地、州、市土地荒漠现状程度 (五个级别 )的评价和制图工作 ,并针对荒漠化程度的差异 ,提出了生态环境保护的措施和建议 ,为全区生态环境的动态监测和管理提供了依据。通过此次监测 ,不仅提高了全区生态环境遥感监测的水平 ,也为…     

新疆艾比湖流域平原区景观植被属性特征研究

在对新疆艾比湖流域平原区进行景观生态分类的基础上，利用“3S”技术叠置研究区草地资源类型图与景观类型图，对研究区景观植被属性特征进行分析。结果表明，研究区主要为荒漠、草原和草甸，共有33个植物群落类型，小蓬荒漠、梭梭荒漠、刚毛柽柳荒漠等各类荒漠面积合计约占研究区总面积的74．10％，芦苇草甸、含胡杨的芦苇草甸及矮嵩草草甸等各类草甸及草原面积也较大，占研究区总面积的18．34％。     

荒漠生态系统监测研究指标体系

新疆环境保护科学研究所自1984年接受“荒漠生态系统监测指标体系的观测研究”课题,在乌鲁木齐北部90km处的沙漠边缘建立了“准噶尔沙漠生态系统定位研究站”,自1987年正式开展了“荒漠生态系统定位观测研究”工作,从古尔班通沙漠中部至天山博格达峰中山带选定了沙漠、沙漠边缘、山前洪冲积扇、前山和中山带五个观测场,沙漠四季进行定位观测,同时,在站内进行多项目的连续观测,现集五年观测研究经验,结合中国科学院及国外研究站的先进经验,建立了荒漠生态系统指标体系。     

新疆干旱区的水环境问题分析及对策

在分析新疆特定的自然地理条件及气修水文特征的基础上，讨论了新疆目前面临的水资源短缺、干旱化、沙漠化加剧；水土流失、土壤盐渍化严重；水污染日益严重、水质恶化等主要的水环境问题，对新疆水资源环境的改善提出了相应的对策。     

新疆生态可持续发展的主要制约因子及脆弱区域分析

自然生态系统的可持续发展是社会一经济系统可持续发展的基本保证，明确区域生态可持续发展的主要制约因子和生态脆弱区域是评价区域生态系统发展的可持续性、制定可持续发展战略及实施综合措施的关键步骤。本文分析了新疆生态可持续发展的主要制约因子和生态脆弱区域。结果表明，水资源危机、土地荒漠化、耕地资源危机及森林减少等是限制新疆生态可持续发展的主要制约因子；干旱绿洲-沙漠过渡地区和内陆河（湖）流域为重点生态脆弱区域。在此基础上，提出了新疆生态系统可持续发展的对策建议。     

荒漠化及其监测

本文通过对荒漠化过程的探讨,提出了荒漠化监测指标体系及监测评价方法,为新疆开展荒漠生态环境监测工作提供依据.     

The use of spatial empirical models to estimate soil erosion in arid ecosystems

The central objective of this project was to utilize geographical information systems and remote sensing to compare soil erosion models, including Modified Pacific South-west Inter Agency Committee (MPSIAC), Erosion Potential Method (EPM), and Revised Universal Soil Loss Equation (RUSLE), and to determine their applicability for arid regions such as Kuwait. The northern portion of Umm Nigga, containing both coastal and desert ecosystems, falls within the boundaries of the de-militarized zone (DMZ) adjacent to Iraq and has been fenced off to restrict public access since 1994. Results showed that the MPSIAC and EPM models were similar in spatial distribution of erosion, though the MPSIAC had a more realistic spatial distribution of erosion and presented finer level details. The RUSLE presented unrealistic results. We then predicted the amount of soil loss between coastal and desert areas and fenced and unfenced sites for each model. In the MPSIAC and EPM models, soil loss was different between fenced and unfenced sites at the desert areas, which was higher at the unfenced due to the low vegetation cover. The overall results implied that vegetation cover played an important role in reducing soil erosion and that fencing is much more important in the desert ecosystems to protect against human activities such as overgrazing. We conclude that the MPSIAC model is best for predicting soil erosion for arid regions such as Kuwait. We also recommend the integration of field-based experiments with lab-based spatial analysis and modeling in future research.     

Assessment of spatial distribution of soil loss over the upper basin of Miyun reservoir in China based on RS and GIS techniques

Soil conservation planning often requires estimates of the spatial distribution of soil erosion at a catchment or regional scale. This paper applied the Revised Universal Soil Loss Equation (RUSLE) to investigate the spatial distribution of annual soil loss over the upper basin of Miyun reservoir in China. Among the soil erosion factors, which are rainfall erosivity (R), soil erodibility (K), slope length (L), slope steepness (S), vegetation cover (C), and support practice factor (P), the vegetative cover or C factor, which represents the effects of vegetation canopy and ground covers in reducing soil loss, has been one of the most difficult to estimate over broad geographic areas. In this paper, the C factor was estimated based on back propagation neural network and the results were compared with the values measured in the field. The correlation coefficient (r) obtained was 0.929. Then the C factor and the other factors were used as the input to RUSLE model. By integrating the six factor maps in geographical information system (GIS) through pixel-based computing, the spatial distribution of soil loss over the upper basin of Miyun reservoir was obtained. The results showed that the annual average soil loss for the upper basin of Miyun reservoir was 9.86 t ha(-1) ya(-1) in 2005, and the area of 46.61 km(2) (0.3%) experiences extremely severe erosion risk, which needs suitable conservation measures to be adopted on a priority basis. The spatial distribution of erosion risk classes was 66.9% very low, 21.89% low, 6.18% moderate, 2.89% severe, and 1.84% very severe. Thus, by using RUSLE in a GIS environment, the spatial distribution of water erosion can be obtained and the regions which susceptible to water erosion and need immediate soil conservation planning and application over the upper watershed of Miyun reservoir in China can be identified.     

梭梭、白梭梭萌发过程的初探

针对准噶尔盆地南部沙漠边缘沙丘活化这一现象,结合目前新疆梭梭、白梭梭研究现状,结合历年的气象资料,模拟自然条件,对梭梭、白梭梭自然恢复的初始过程——种子萌发的温度和水分条件进行研究。结果表明,新疆梭梭、白梭梭种子在2℃时就可以萌发,而且发芽率达80%以上,当积雪厚度达到22 cm时,梭梭、白梭梭种子发芽率达到80%以上,变温提高发芽速率,当积雪厚度达到22 cm就可满足梭梭、白梭梭种子萌发的水分条件。此结果可为沙漠地区植被自然恢复提供理论依据。     

伊犁低山丘陵区小流域水土保持措施优化配置研究

在调查分析伊犁低山丘陵区水土流失特点的基础上，研究了该区小流域水土保持措施的空间配置。结果表明：伊犁低山丘陵区水土流失主要表现为以水力侵蚀为主的多种土壤侵蚀类型作用下的坡面侵蚀和沟道侵蚀。针对其水土流失特点，伊犁低山丘陵区小流域水土保持措施优化配置为：以生态修复为主，上游地区封禁保护；中游地区种植水保林和经济林带，建立生态缓冲带；下游水平沟种草。通过综合治理开展水土保持生态环境建设，至2012年底，伊犁低山丘陵区治理程度达到77．33％，林草覆盖率48％，改善了当地生态环境。     

An assessment to prioritise the critical erosion-prone sub-watersheds for soil conservation in the Gumti basin of Tripura,North-East India

Erosion-induced land degradation problem has emerged as a serious environmental issue across the world. Assessment of this problem through modelling can generate valuable quantitative information for the planners to identify priority areas for proper soil conservation measures. The Gumti River basin of Tripura falls under humid tropical climate and experiences soil erosion for a prolonged period which has turned into a major environmental issue. Increased sediment supply through top soil erosion is one of the major reasons for reduced navigability of this river. Thus, the present study is an attempt to prioritize the sub-watersheds of the Gumti basin by estimating soil loss through the USLE (Universal Soil Loss Equation) model. For that purpose, five parameters of the USLE model were processed, computed and overlaid in a GIS environment. The result shows that potential mean annual soil loss of the Gumti basin ranges between 0.03 and 114.08 t ha^?1 year^?1. The resultant values of soil loss were classified into five categories considering the minimum and maximum values. It has been identified that low, moderate, high, very high and severe soil loss categories occupy 68.71, 8.94, 5.86, 5.02 and 11.47% of the basin respectively. Moreover, it has been recognised that sub-watersheds like SW7, SW8, SW12, SW21, SW24 and SW29 fall under very high priority class for which mitigation measures are essential. Therefore, the present study recommends mitigation measures through terrace cultivation, as an alternative of shifting cultivation in the hilly areas and through construction of check dams at the appropriate sites of the erosion prone sub-watersheds. Moreover, proper afforestation programmes that have been implemented successfully in other parts of Tripura through the Japan International Cooperation Agency, Joint Forest Management, and National Afforestation Programme should be initiated in the highly erosion-prone areas of the Gumti River basin.     

新疆北部沙漠边缘植被恢复可能性初探

古尔班通古特沙漠边缘植被破坏严重,沙丘活化明显,是新疆干旱植被恢复的重点地区之一,一般缺乏地表水补充,其沙丘的水分状况便成为植被生存和恢复过程的关键条件,为探究古尔班通古特沙漠边缘植被恢复的可能性,在植物生长期内对流动沙丘和固定沙丘不同部位的水分状况进行了连续监测,结果表明:沙丘大多数层次含水量月变化与月降水量分布相一致;流动沙丘含水量从上部到下部依次升高;流动沙丘中部和下部稳定湿沙层处在距沙丘表面60 cm以下,且厚度超过100 cm,固定沙丘稳定湿沙层只存在于沙丘中部距沙丘表面60～150 cm内,其厚度不超过100 cm,在一般年份,该地区利用本地种进行植被恢复是可行的.     

Morphometry and land cover based multi-criteria analysis for assessing the soil erosion susceptibility of the western Himalayan watershed

Complex mountainous environments such as Himalayas are highly susceptibility to natural hazards particular those that are triggered by the action of water such as floods, soil erosion, mass movements and siltation of the hydro-electric power dams. Among all the natural hazards, soil erosion is the most implicit and the devastating hazard affecting the life and property of the millions of people living in these regions. Hence to review and devise strategies to reduce the adverse impacts of soil erosion is of utmost importance to the planners of watershed management programs in these regions. This paper demonstrates the use of satellite based remote sensing data coupled with the observational field data in a multi-criteria analytical (MCA) framework to estimate the soil erosion susceptibility of the sub-watersheds of the Rembiara basin falling in the western Himalaya, using geographical information system (GIS). In this paper, watershed morphometry and land cover are used as an inputs to the MCA framework to prioritize the sub-watersheds of this basin on the basis of their different susceptibilities to soil erosion. Methodology included the derivation of a set of drainage and land cover parameters that act as the indicators of erosion susceptibility. Further the output from the MCA resulted in the categorization of the sub-watersheds into low, medium, high and very high erosion susceptibility classes. A detailed prioritization map for the susceptible sub-watersheds based on the combined role of land cover and morphometry is finally presented. Besides, maps identifying the susceptible sub-watersheds based on morphometry and land cover only are also presented. The results of this study are part of the watershed management program in the study area and are directed to instigate appropriate measures to alleviate the soil erosion in the study area.     

基于RS和GIS的干旱荒漠区域土壤侵蚀动态监测与评价

为建立土壤侵蚀动态变化数据库，本文以土地利用数据、植被覆盖指数、最大风速等值线图和DEM数据为信息源，对干旱荒漠区新疆克拉玛依市2000年和2007年的土壤侵蚀状况进行了动态监测与评价。结果表明，受自然条件和人类活动影响，8年间克拉玛依市土壤侵蚀强度有所增加，变化区域主要集中在克拉玛依市中部平原区。该方法的应用实现了土壤侵蚀的定时定量评价。     

黑龙江流域水环境背景值研究进展

黑龙江流域地处世界三大黑土区之一的中国东北平原，土壤腐殖质含量高，这些腐殖质随着地面径流进入水体，成为流域溶解性有机物（DOM）的自然本底（环境背景）。自然本底的存在导致流域水质有机污染综合指标不能真实反映流域的人为污染，流域背景区内高锰酸盐指数、化学需氧量背景值范围分别为3.0~11.7、14.3~40.5 mg/L。流域部分水质考核断面水质受到有机质背景值的影响。由于叠加人为污染，定量分析高锰酸盐指数、化学需氧量背景值范围存在很大难度。重金属元素相对稳定，相对于"六五"时期重金属背景值，目前水体中重金属含量普遍升高。结合水环境管理需求，背景值研究成果应用于水环境管理还需要进一步深入研究和实践。笔者在综述黑龙江流域水环境背景值研究基础上，总结目前存在的问题，提出水环境背景值研究建议，为科学客观评价流域水质提供参考。