南水北调中线水源地汉江上游流域主要生态环境问题及对策

汉江上游是南水北调中线水源地，流域生态环境建设是保障水源地水质安全的关键。针对上游流域水环境污染、土地利用以及水土流失等重大生态环境问题，结合流域数字高程模型及水质调查对其进行了系统分析。结果表明：（1）丹江流域、库区流域及汉中盆地水质较差，CODMn和氨氮成为水源区主要污染物；（2）各子流域区植被覆盖占各自面积的712%~957%，表明流域植被覆盖较好，但沿河岸100 m范围内农业用地占292%~434%，且多为坡耕地；（3）流域水土流失严重，2000年左右流域侵蚀图显示汉江源头、秦岭南及大巴山北均出现了大片年均侵蚀模数>2 200 t/km2的区域，且有日益增强的趋势。提出加大水环境污染整治力度、加强农业用肥管理及河岸带建设、水土保持建设以及加强流域水环境及水土保持监测和科研工作等对策。     

下游集中补给型泥石流动力学特征与防治对策——以四川省泸定县干沟泥石流为例

干沟泥石流是一条典型的下游集中补给型泥石流沟,其物源的启动、流通与堆积在700 m范围内完成.以2005年干沟泥石流过程为例,应用三种计算公式对该沟泥石流的动力学参数进行了计算.通过计算发现,三种公式计算结果差别不大,并取其平均值作为计算结果.根据干沟泥石流流量计算和形态调查对比分析,认为2005年干沟泥石流的形成过程具有明显的堵溃效应,且前期降雨对泥石流的发生影响较为明显.在对干沟泥石流动力学参数计算、物源补给特征及形成过程分析的基础上,认为干沟在2005年后易形成高频泥石流,对该沟泥石流开展监测预警尤为必要,提出了该沟泥石流监测预警方式并予以实施,可为干沟泥石流的防灾减灾提供科学依据.     

Quantitative modeling of freshwater stress in the nine water basins of Tanzania

Freshwater scarcity is a global issue of environmental concern that threatens agricultural production and human health. In this study, we established freshwater stress indices (WSIs) for the nine water basins of Tanzania by using the quantity of freshwater available and various water uses. The relationship between water availability and different water uses, including environmental water requirements, was analyzed, with uncertainty and sensitivity analysis performed by a Monte Carlo simulation technique. Extreme WSI values close to 1.00 were obtained in the Rufiji, Pangani, and Wami-ruvu basins, Internal drainage, and Lake Rukwa, while low and moderate WSI values ranging from 0.03 to 0.84 were found in Lake Victoria and the Ruvuma, Tanganyika, and Nyasa basins. This study adds further knowledge on the level of freshwater scarcity, relationships between water availability and different water uses, and suggests policy options to reduce freshwater scarcity at the basin level for sustainable water supply.     

四川省人口增长与主要生态资源承载力研究

本文以个体生活资源基本需求为计算单位,探讨四川省主要生态资源能承载多少人口,预测四川省人口发展与生态资源的关系.根据本文给出的计算结果,四川省耕地费源已经饱和,其复耕事较高尚能满足人口需求;牧草场资源超载,面临荒漠化威胁;森林资源较为丰富,能够满足人口发展需求;水资源与人口关系富足有余,但工业污水排放和上游水源保护仍需给予关注.面对这一现实,四川省要进一步推行控制人口增长的生育政策;保护现有耕地资源,发展生态农业;合理规划草场资源,科学发展畜牧业;合理开发森林蕴藏资源,坚持合理采伐;加强水利设施建设,防治水污染,确保水资源可持续利用.     

流域水体生态修复技术探讨

针对河道等自然流域的水体污染物进行生态治理,作者提出运用三个独立步骤而形成一道自然水体修复功能：第一步,优选良性微生物株群并持续发展与供给;第二步,运用河道功能增加水中的溶解氧;第三步,建立流域水体生物链,从而达到流域水体消纳污染物的自净效果。     

Estimating Annual Groundwater Evapotranspiration from Phreatophytes in the Great Basin Using Landsat and Flux Tower Measurements

Escalating concerns about water supplies in the Great Basin have prompted numerous water budget studies focused on groundwater recharge and discharge. For many hydrographic areas (HAs) in the Great Basin, most of the recharge is discharged by bare soil evaporation and evapotranspiration (ET) from phreatophyte vegetation. Estimating recharge from precipitation in a given HA is difficult and often has significant uncertainty, therefore it is often quantified by estimating the natural discharge. As such, remote sensing applications for spatially distributing flux tower estimates of ET and groundwater ET (ET_g) across phreatophyte areas are becoming more common. We build on previous studies and develop a transferable empirical relationship with uncertainty bounds between flux tower estimates of ET and a remotely sensed vegetation index, Enhanced Vegetation Index (EVI). Energy balance‐corrected ET measured from 40 flux tower site‐year combinations in the Great Basin was statistically correlated with EVI derived from Landsat imagery (r² = 0.97). Application of the relationship to estimate mean‐annual ET_g from four HAs in western and eastern Nevada is highlighted and results are compared with previous estimates. Uncertainty bounds about the estimated mean ET_g allow investigators to evaluate if independent groundwater discharge estimates are “believable” and will ultimately assist local, state, and federal agencies to evaluate expert witness reports of ET_g, along with providing new first‐order estimates of ET_g.     

ESTIMATING PARAMETERS OF EV1 DISTRIBUTION FOR FLOOD FREQUENCY ANALYSIS1

ABSTRACT: The parameters of the extreme value type 1 distribution were estimated for 55 annual flood data sets by seven methods. These are the methods of (1) moments, (2) probability weighted moments, (3) mixed moments, (4) maximum likelihood estimation, (5) incomplete means, (6) principle of maximum entropy, and (7) least squares. The method of maximum likelihood estimation was found to be the best and the method of incomplete means the worst. The differences between the methods of principle of maximum entropy, probability weighted moments, moments, and least squares were only minor. The difference between these methods and the method of maximum likelihood was not pronounced.     

滇池流域水资源的开发与保护

本文介绍了滇池流域的自然条件和社会经济发展,分析了水资源特点,对其开发现状和供需预测作了评述,并提出了进一步开发和保护水资源的建议。     

A historical perspective of river basin management in the Pearl River Delta of China

Three innovations in water and soil conservancy technology in the Pearl River Delta of South China, i.e., dike building, land reclamation, and dike-pond systems, were examined from a historical perspective. They were found to best reflect local farmers' efforts to cope with the challenges of various water disasters and to build a harmonious relationship with the changed environment. These technologies were critical to the agricultural success and sustainability over the past 2000 years, and reflected local farmers' wisdom in balancing land use and environmental conservation. Imprudent use of a new agricultural technology could damage the environment, and could disturb the human-environment relationship, as evidenced by the more frequent flooding that followed inappropriate dike building and premature reclamation. It is suggested that as the urbanization and industrialization process in the delta region continues, the kind of thinking that made the water and soil conservancy sustainable needs to be incorporated into the design of similar technologies for water use and river basin management today.     

川中丘陵紫色土区农田土壤有机碳储量及空间分布特征

土壤有机碳在陆地生态系统碳循环中起着举足轻重的作用。针对农田区域内典型县域尺度有机碳储量及其空间格局特征的研究,可以为区域农田土壤固碳提供参考,为研究我国土壤有机碳储量提供基础数据支持。基于2012年农田土壤有机碳分析调查数据,结合GIS和GPS技术对川中丘陵区盐亭县土壤有机碳密度和储量及空间格局进行了估算和分析。结果表明:其主要土壤类型的0~20 cm耕层土壤有机碳密度为111~426 kg/m2,平均值为266 kg/m2,水田和旱地耕层土壤有机碳密度分别为345和234 kg/m2,均低于全国平均值;全县20 cm深度土壤有机碳总储量250×109 kg C,紫色土类土壤有机碳储量最大,为153×109kg C,水稻土次之,有机碳储量0.93×109kg C,两者占据了农田土壤有机碳储量约98%,冲积土和黄壤土类由于面积小,有机碳储量也最低。各土壤类型有机碳储量丰度指数(RI)值都较低,碳存储能力处于中下水平。在县域农田尺度,有机碳空间格局与气候差异、植被类型关系不大,土壤类型空间差异和地形差异是有机碳空间格局形成的主要原因。