大型水利工程对洞庭湖区水资源开发利用的影响

洞庭湖区北靠长江,南汇湘、资、沅、澧四水,水资源总量相对丰富,然而近年来在气候变化与人类活动的双重驱动下,开始呈现"旱涝并存、旱涝交替"的特征,水资源供需矛盾逐渐加剧。为探讨上游大型水利工程(主要为三峡工程与四水流域控制性枢纽工程)的运行对洞庭湖区水资源开发利用的影响,结合近50a来长江干流及四水水位与水资源情势的演变规律和总体趋势,对比分析了不同时间节点下洞庭湖区水位与水资源总量的年际、年内变化特征,以期从众多的影响因子中辨识出大型水利工程的影响,为湖区水资源的合理开发与保护提供一定依据。结果表明:三峡工程建成运行初期,对于洞庭湖区的水资源开发利用产生了一定的不利影响,且影响主要集中在荆南三口地区,而四水工程的影响相较之下并不显著。     

黄土滑坡稳定性评价的反演分析

本文根据黄土滑坡的变形监测结果，同时考虑了边坡的初期应变分布状况，通过有限元反分析法，反推出边坡地基的力学参数，为黄土滑坡的稳定性评价和预报提供了可靠的依据。     

四湖地区水资源及其调控

四湖地区是湖北省有名的“水袋子”,治水是关系社会经济发展的重大问题。该区降水丰沛,年均１１１５．３ｍｍ,产生径流深３４３．８ｍｍ;过境客水流量大,年均５０８８×１０８１ｍ３;总体水资源丰富。由于降水的时空分布不匀,客水流量不稳定,常造成来水集中而形成洪涝灾害,来水不足而形成干旱威胁,尤其是春旱。建国以来,为兴利去害,四湖地区经历了隔断江湖、疏理水系、建立引水与自排系统、以及修建电排站等以防洪、排涝和灌溉为主要目的大规模水系整治过程,有效地控制了流域水患。但同时促进了过度的围湖围垸垦殖,使调蓄能力锐减,外洪内涝不断,所造成的经济损失也越来越大。在进一步分析了四湖地区洪涝灾害频繁发生的内外原因之后,提出了加固堤防,完善分蓄洪区建设;调整土地利用结构,合理调蓄;完善设施,合理调度的水资源调控对策措施。     

Prioritizing Wetland Restoration for Sediment Yield Reduction: A Conceptual Model

In a climate of limited resources, it is often necessary to prioritize restoration efforts geographically. The synoptic approach is an ecologically based tool for geographic prioritization of wetland protection and restoration efforts. The approach was specifically designed to incorporate best professional judgment in cases where information and resources are otherwise limited. Synoptic assessments calculate indices for functional criteria in subunits (watersheds, counties, etc.) of a region and then rank the subunits. Ranks can be visualized in region-scale maps which enable managers to identify areas where efforts optimize functional performance on a regional scale. In this paper, we develop a conceptual model for prioritizing watersheds whose wetlands can be restored to reduce total sediment yield at the watershed outlet. The conceptual model is designed to rank watersheds but not individual wetlands within a watershed. The synoptic approach is valid for applying the sediment yield reduction model because there is high demand for prioritizing disturbed wetlands for restoration, but there is limited, quantitative, accurate information available with which to make decisions. Furthermore, the cost of creating a comprehensive database is prohibitively high. Finally, because the model will be used for planning purposes, and, specifically, for prioritizing based on multiple decisions rather than optimizing a single decision, the consequence of prioritization errors is low. Model results cannot be treated as scientific findings. The conclusions of an assessment are based on judgement, but this judgement is guided by scientific principles and a general understanding of relevant ecological processes. The conceptual model was developed as the first step towards prioritizing of wetland restoration for sediment yield reduction in US EPA Region 4.     

结构红利与资源诅咒——西部大开发以来内蒙古产业结构变迁绩效评价

统计分析表明，西部大开发以来内蒙古经济存在越来越严重的就业-产值结构偏离趋势。采用shilt—share方法分别对西部大开以来内蒙古、西部和全国的劳动生产率进行分解和比较分析发现，内蒙古的结构红利不显著。因此，近年来内蒙古经济虽有良好的增长绩效，但其资源依赖型增长正通过价格机制和制度效率两个途径制约着产业结构的高级化与合理化变迁，即存在潜在的资源诅咒问题。     

京津冀地区面向人居环境之水安全格局初探

采用文献法对近年京津冀水资源、水环境、水污染、水灾害、水管理等水安全情势进行相关数据分析,从总体上显示出水危机问题和京津冀地区快速城市化发展的关联性.结果表明:1)京津冀城市群必须向节水型社会模式转型;2)建立区域及城市间的协调机制,才能有效克服流域与区域等级的水问题;3)实现京津冀地区水安全格局的治理行动计划网络,提出保护恢复体系、净化循环体系、限制节约体系、调度再造体系、蓄滞防洪减灾体系五大体系.     

基于MODIS GPP/NPP数据的三江源地区草地生态系统碳储量及碳汇量时空变化研究

陆地生态系统碳循环研究是全球变化与地球科学研究领域的前沿与热点问题,准确地评估陆地生态系统碳储量和碳汇量是估算未来大气 CO2浓度,预测气候变化及其对陆地生态系统影响的关键。已有相关研究多集中于对区域生态系统碳储量和碳汇量的量的估算,而缺乏针对时间尺度上的变化过程的分析,以及对变化特征空间差异性的分析。本研究基于MODIS NPP数据,结合土地利用数据及土壤有机碳密度分布数据,对三江源地区2000─2010年草地生态系统碳储量时空变化特征进行了分析,同时,基于MODIS GPP数据及China FLUX和America FLUX数据,建立草地生态系统呼吸估算模型,对其碳汇量的时空变化特征进行了分析,以期明确该地区的碳储存能力及其变化过程,为该区域草地生态系统保护和管理提供科学依据。研究结果表明：（1）三江源地区草地生态系统总碳储量为53.38×108 t,平均碳密度为14.94 kg·m-2（以C计）。土壤和植被碳储量分别为53.07×108 t和0.31×108 t,平均碳密度分别为14.85 kg·m-2和86.77 g·m-2。（2）近10多年来,三江源地区草地生态系统多年平均碳汇量为0.4×108 t,单位面积平均碳汇量为86.80 g·m-2·a-1（以C计）,表明该地区草地生态体统是一个碳汇。（3）2000年以来,三江源地区草地生态系统总碳储量及总碳汇量均呈波动增加趋势,碳汇功能有所增强。（4）三江源地区草地生态系统碳储量及碳汇量的空间分布格局及其变化趋势的空间分布均呈现明显的空间差异性。（5）MODIS GPP/NPP数据能够支撑较大尺度草地生态系统碳储量及碳汇量格局与变化趋势分析,较传统方法更为便捷高效。     

Conceptual Models as Hypotheses in Monitoring Urban Landscapes

Many problems and challenges of ecosystem management currently are driven by the rapid pace and spatial extent of landscape change. Parks and reserves within areas of high human population density are especially challenged to meet the recreational needs of local populations and to preserve valued environmental resources. The complex problem of managing multiple objectives and multiple resources requires an enormous quantity of information, and conceptual models have been proposed as tools for organizing and interpreting this information. Academics generally prefer a bottom-up approach to model construction that emphasizes ecologic theory and process, whereas managers often use a top-down approach that takes advantage of existing information to address more pragmatic objectives. The authors propose a formal process for developing, applying, and testing conceptual models to be used in landscape monitoring that reconciles these seemingly opposing perspectives. The four-step process embraces the role of hypothesis testing in the development of models and evaluation of their utility. An example application of the process to a network of national parks in and around Washington, DC illustrates the ability of the approach to systematically identify monitoring data that would both advance ecologic theory and inform management decisions.     

因子回归和交互联合探索区域植被覆盖度的影响因素——以三江源地区为例

利用SPOT VEGETATION数据获取的归一化植被指数（NDVI）,分析三江源地区植被覆盖度（FVC）的空间异质性,围绕自然和人类活动因素,基于因子回归与交互作用联合探索自然因素和人为因素对三江源地区植被覆盖的影响.结果表明：（1）三江源地区植被覆盖度整体呈现明显的空间异质性;（2）总体上FVC空间分布的影响因素表现为自然环境因素>人类活动因素;（3）降水是影响三江源地区FVC的主要驱动因子,解释力达0.777;（4）因子交互发现：驱动解释系统呈现双因子增强,说明从系统的角度来看不存在独立起作用的因子,年降水量与其他因子的交互作用最强;（5）降水梯度影响了三江源地区FVC空间异质性的解释程度.随着降水增加,因子解释力趋稳,在降水量较多的三江源东部地区,FVC趋向于更易受高程和气温的影响;（6）数据结果亦验证了因子独立的全局最优筛选仅仅是模拟因变量特征的最优函数,其解释效果与因变量的驱动解释不能完全等同.     

黄土高原大气降水δ18O的空间分布

大气降水δ¹⁸O值的空间分布可以为理解现代大气中的水分输送提供空间信息,也可以为解释古气候代用指标的环境意义提供基础。本文整理了黄土高原44个站点的实测降水δ¹⁸O数据,基于纬度和海拔构建回归模型并得到了黄土高原降水δ¹⁸O的同位素景观图谱,结合实测资料和图谱结果分析了降水δ¹⁸O的年内变化和空间分布特征,并评价了两种全球降水同位素景观图谱产品的适用性,得出以下结论：（1）黄土高原降水δ¹⁸具有明显的年内变化特征,春夏季相对富集,秋冬季较为贫化。（2）黄土高原降水δ¹⁸O高值区多出现在南部的渭河谷地一带,低值区则主要出现在西部高原山地和北部边缘。（3）黄土高原北部与西部降水δ¹⁸温度效应更为明显,向南和向东延伸,温度效应逐渐弱化。（4）两种全球降水同位素景观图谱产品对δ¹⁸值的最佳模拟结果均出现在夏季,冬季模拟较差。