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491.
为了定量分析和比较区域生态服务功能及其价值变化,运用中国生态系统服务价值当量因子表和岷江上游流域单位面积农田生态系统提供的食物生产服务的经济价值,以及分析1986、1995和2000年三期TM遥感影像所得到的土地利用情况,对岷江上游地区不同年代的生态服务价值变化进行了估算和比较。并初步分析了生态服务价值变化的原因。1986~1995年,农田面积增加了60 801 hm2,比1986年增长了477%。林地面积减少了89 01217 hm2,占原来面积的497%。总的生态服务价值从1986年到2000年减少了1199×108元。主要是由于人口的增加和森林的砍伐,导致森林面积减少,转变为草地、农田等土地利用类型。通过1995年和2000年对比得出:自从1998年实施“天然林保护工程”政策以来,到2000年森林生态系统面积与1995年相差约4 16528 hm2,生态服务价值相差约79亿元,可见国家政策在保护生态系统服务功能上虽起到了一定的作用,但与1986年相比还相差甚远,天然林保护工程任重而道远。  相似文献   
492.
生态系统变化对岩溶水资源的影响--以湘西为例   总被引:17,自引:3,他引:17  
岩溶水资源是支撑岩溶区社会经济发展最为重要的一个基本方面,明确生态系统变化是如何影响岩溶水资源的质与量这一重大问题,将有助于岩溶水循环机制的深入研究,为揭示岩溶水资源的形成、演化规律及控制机理,建立岩溶水资源评价、开发利用和保护的系统理论,探索岩溶水资源可持续利用模式提供科学的依据。在分析岩溶山区典型生态系统类型及其演化特征和岩溶水资源特点的基础上,通过湘西20年来的生态系统变化的对比,就其对岩溶水资源的影响进行了详细的论述。认为生态的恶化是引起岩溶石山区水资源短缺的一个重要因素,生态系统变化对岩溶水资源的影响主要是通过对岩溶水的补给、径流、排泄等的影响,使岩溶水资源产生水质和水量的变化。  相似文献   
493.
Ecosystem risk is a new concept in understanding environmental problems. It is important to study and develop quantitative methods for regional ecosystem risk analysis. In this study, some new indicators and methods for measuring oasis ecosystem risk were established using reliability theory. These indicators are linked to water resource, which is the key restricting factor in arid area oasis ecosystems. They have clear meanings and can also be compared in different arid area oases. A case study in the Liangzhou oasis of the Shiyang River Basin in China shows how to calculate these ecosystem risk indicators. The results of the case study are as follows: the reliability indicator, risk indicator, stability indicator, and integrated loss indicator of the Liangzhou oasis are 0.686, 0.314, 0.743, and 0.301, respectively. This means that the reliability degree of the oasis's ecosystem safety is 68.6%; the degree of risk that it is unsafe is 31.4%; the stability degree is 74.3%; and 30.1% of the oasis's area is supported by over-exploiting underground water and damaging the lower reaches of the ecosystem. This result can be used as a guide in controlling and managing ecosystem risk in the research area.  相似文献   
494.
生态系统服务功能价值评估方法综述   总被引:31,自引:0,他引:31  
本文在回顾生态系统服务功能价值分类和评估方法的基础上,得出目前我国的生态系统服务功能价值评估方法正处于从学习、模仿向渐进成熟阶段过渡,通过对生态系统服务功能的价值评估方法的对比分析,得出生态系统功能价值评估方法选择应根据先直接市场法、再替代市场法、最后模拟市场法的基本原则进行.  相似文献   
495.
Abstract: Cumulatively, headwater streams contribute to maintaining hydrologic connectivity and ecosystem integrity at regional scales. Hydrologic connectivity is the water‐mediated transport of matter, energy and organisms within or between elements of the hydrologic cycle. Headwater streams compose over two‐thirds of total stream length in a typical river drainage and directly connect the upland and riparian landscape to the rest of the stream ecosystem. Altering headwater streams, e.g., by channelization, diversion through pipes, impoundment and burial, modifies fluxes between uplands and downstream river segments and eliminates distinctive habitats. The large‐scale ecological effects of altering headwaters are amplified by land uses that alter runoff and nutrient loads to streams, and by widespread dam construction on larger rivers (which frequently leaves free‐flowing upstream portions of river systems essential to sustaining aquatic biodiversity). We discuss three examples of large‐scale consequences of cumulative headwater alteration. Downstream eutrophication and coastal hypoxia result, in part, from agricultural practices that alter headwaters and wetlands while increasing nutrient runoff. Extensive headwater alteration is also expected to lower secondary productivity of river systems by reducing stream‐system length and trophic subsidies to downstream river segments, affecting aquatic communities and terrestrial wildlife that utilize aquatic resources. Reduced viability of freshwater biota may occur with cumulative headwater alteration, including for species that occupy a range of stream sizes but for which headwater streams diversify the network of interconnected populations or enhance survival for particular life stages. Developing a more predictive understanding of ecological patterns that may emerge on regional scales as a result of headwater alterations will require studies focused on components and pathways that connect headwaters to river, coastal and terrestrial ecosystems. Linkages between headwaters and downstream ecosystems cannot be discounted when addressing large‐scale issues such as hypoxia in the Gulf of Mexico and global losses of biodiversity.  相似文献   
496.
Abstract: Headwater streams make up a large proportion of the total length and watershed area of fluvial networks, and are partially characterized by the large volume of organic matter (large wood, detritus, and dissolved organic matter) and invertebrate inputs from the riparian forest, relative to stream size. Much of those inputs are exported to downstream reaches through time where they potentially subsidize river communities. The relative rates, timing, and conversion processes that carry inputs from small streams to downstream reaches are reasonably well quantified. For example, larger particles are converted to smaller particles, which are more easily exported. Also, dissolved organic matter and surface biofilms are converted to larger particles which can be more easily intercepted by consumers. However, the quality of these materials as it affects biological activity downstream is not well known, nor is the extent to which timing permits biological use of those particles. These ecological unknowns need to be resolved. Further, land uses may disrupt and diminish material transport to downstream reaches by removing sources (e.g., forest harvest), by affecting transport and decomposition processes (e.g., flow regulation, irrigation, changes in biotic communities), and by altering mechanisms of storage within headwaters (e.g., channelization). We present conceptual models of energy and nutrient fluxes that outline small stream processes and pathways important to downstream communities, and we identify informational gaps that, if filled, could significantly advance the understanding of linkages between headwater streams and larger rivers. The models, based on empirical evidence and best professional judgment, suggest that navigable waters are significantly influenced by headwater streams through hydrological and ecological connectivities, and land use can dramatically influence these natural connectivities, impacting downstream riverine ecosystems.  相似文献   
497.
康凤琴  张杰  王静 《灾害学》2007,22(3):49-52,62
通过分析百年尺度上中国西北降水空间分布规律和沙漠界线、农牧交错带界线的演变规律,认为:①干旱、半干旱是西北地区的主要气候特征;②生态系统非常敏感和脆弱;③在维持温饱和经济利益驱动下建立的农、牧业产业结构,是造成西北环境恶化的最主要的原因。  相似文献   
498.
In a total of 189 water samples collected from Danish streams no traces of the pyrethroid esfenvalerate were detected. However, pyrethroids have previously been found in sediments in 9 out of 30 streams investigated. We found that the shredding activity of the Trichopteran Sericostoma personatum and the amphipod Gammarus pulex was significantly reduced with increased concentration of the pyrethroid lambda-cyhalohtrin adsorbed to the leaves on which they fed. Predation rate on the Plecopteran Leuctra nigra by the leech Erpobdella octoculata increased significantly with increasing concentration of lambda-cyhalothrin on the leaves on which L. nigra was fed. Our results clearly indicate that the ongoing monitoring of pesticides is likely to underestimate pyrethroid occurrence and that sediment-bound pyrethroids have a potential negative impact on ecosystem function and biotic interactions in streams.  相似文献   
499.
基于土地利用变化的生态服务价值损益估算--以大庆市为例   总被引:21,自引:0,他引:21  
土地利用/覆盖变化遥感研究表明,大庆市自1988年以来土地利用状态变化很大,由此引起了该区域生态环境的一系列响应及其生态系统服务价值的变化。以大庆市1988年和2001年的Landsat TM图像解译数据为基础,应用Costanza等人对全球生态系统服务价值的测算方法,分析了该市土地利用变化及其所引起的生态系统服务价值的变化。研究结果表明,13年间,大庆市土地利用的变化损害了该区域生态系统的生态服务功能,使生态系统服务价值损失了20.76%-24.01%。  相似文献   
500.
田间增强UV-B辐射对麦田生态系统Fe营养和累积的影响   总被引:4,自引:0,他引:4  
研究大田栽培和自然光条件下,模拟UV-B辐射(UV-B,280nm ~315nm )增强对麦田生态系统Fe营养和累积的影响.在4 个生育期中,UV-B辐射显著增加叶和穗Fe含量,显著降低根Fe 含量,并改变茎Fe 含量.叶Fe累积对UV-B辐射的响应有明显的生育期之间的差异. 分蘖期无显著变化,拔节期和扬花期显著增加,而成熟期显著降低.在各生育期,UV-B辐射显著降低叶、根和穗Fe累积.UV-B辐射显著降低春小麦不同生育期Fe总累积,在5.31kJ·m-2 UV-B辐射下,降低最显著.UV-B辐射还降低春小麦群体Fe输出.麦田土壤速效Fe含量增加是春小麦群体Fe输出降低的结果,可能导致土壤库中Fe 储量的增加.  相似文献   
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