基于GIS长江口北港河段冲淤变化的可视化分析

利用GIS技术,建立长江口北港1973~2003年间不同时期的水下数字高程模型,以此作为基础资料,通过叠合分析不同时期的水下地形图,得到长江口北港不同时段相对的河床冲淤分布图.分析了长江口北港30年来河道的冲淤变化和演变情况,并计算了河道泥沙冲淤量.结果表明,GIS技术是研究河床演变规律的一种行之有效的可视化方法;北港河段在1973~2003年间整体呈冲刷之势,泥沙冲刷量为1.58亿m3,平均每年冲刷0.05亿m3;北港河床航道稳定性较差,受南、北港分汊口演变的影响,北港河床逐渐演变.洪水在北港河槽演变过程中起着重要的作用.     

漳州市河口污染物输入对近岸海域水体富营养化的影响

根据2003～2005年对福建省漳州市入海河口（漳江口、东溪口）和近岸海域（东山湾、宫口湾）的监测调查资料，分析研究了入海河口污染物输入对近岸海域水体富营养化的影响，结果表明：河流陆源的有机、氮、磷污染物入海通量越大，所对应的近岸海域海水水质越差，富营养化趋势越明显．     

治理黄河泥沙的新途径——小北干流放淤

介绍了黄河泥沙的主要来源及危害,提出了治理黄河泥沙的新举措——小北干流放淤,分析了小北干流放淤的客观性和必要性,指出了小北干流放淤对黄河治理的长远影响。     

感潮河道水环境容量理论及计算的若干问题

介绍了感潮河道水环境容量理论及计算的研究现状,分析了存在的主要问题,提出了开展闽江下游河道水环境容量研究的初步设想.     

引黄工程信息系统网络安全的分析

山西省万家寨引黄工程管理局信息系统初步建成，网络安全采用了防火墙、防病毒系统、入侵检测、信息加密、漏洞扫描等防范措施，但仍然存在诸多网络安全的隐患。通过建立物理隔离系统、拨号监控系统，完善防火墙、防杀病毒系统、入侵检测系统、漏洞扫描系统．引黄工程信息系统将成为全方位的安全体系，整个网络将畅通无阻，为引黄工程的生产及办公提供方便快捷的服务。     

新疆塔里木河湿地保护和建设的研究

新疆塔里木河湿地是我国最长的内陆河流湿地,是多种鸟类栖息与多种候鸟迁徙中转、繁殖的重要区域.本文对塔里木河湿地的基本特征、生态功能、近代变化和其保护与建设的现实意义进行了研究,指出应该重视科学研究,拯救珍稀濒危物种,并提出了相应对策.     

Differences between dynamics factors for interannual and decadal variations of rainfall over the Yangtze River valley during flood seasons

The prediction of rainfall in the Yangtze River valley, especially, during flood seasons is the main means for scientists in China working on and the understanding of rainfall-associated processes is a crucial component of this effort. It can be derived f…     

SHRIMP zircon U-Pb dating for volcanic rocks of the Dasi Formation in southeast Hubei Province, middle-lower reaches of the Yangtze River and its implications

The Jinniu Basin in southeast Hubei,located at the westernmost part of middle-lower val-ley of the Yangtze River,is one of the important vol-canic basins in East China. Volcanic rocks in the Jin-niu Basin are distributed mainly in the Majiashan Formation,the Lingxiang Formation and the Dasi Formation,consisting of rhyolite,basalt and basaltic andesite,(trachy)-basalt and basaltic trachy-andesite and (trachy)-andesite and (trachy)-dacite and rhyolite respectively,in which the Dasi volcanism is volumet-rically dominant and widespread. The Dasi volcanic rocks were selected for SHRIMP zircon U-Pb dating to confirm the timing of volcanism. The results indi-cate that there exist a large amount of magmatic zir-cons characterized by high U and Th contents in the volcanic rocks. The concordia ages for 13 points are 128 ± 1Ma (MSWD = 3.0). On account of the shape of zircons and Th/U ratios,this age is considered to represent the crystallization time of the Dasi volcan-ism. The volcanic rocks in the Dasi,Majiashan and Lingxiang Formations share similar trace elementand REE partition patterns as well as Sr-Nd isotopic compositions. In combination with the regional geol-ogy,it is proposed that the southeast Hubei volcanic rocks were formed mainly during the Early Creta-ceous,just like other volcanic basins in middle-lower Yangtze valley. A lithospheric extension is also sug-gested for tectonic regime in this region in the Cre-taceous Period.     

Response of downstream sediment to water resource development in mainstream of the Lancang River

The impact of hydropower cascades of the Lancang River on downstream sedimentation has become one of the key problems in the research of the transboundary water resource development and its possible environmental effects. In this paper, the newest sediment data series spanning 17 years （1987-2003） at Yunjinghong hydrometric station and Chiang Saen hydrometric station, in northern Thailand, are analyzed to reveal these effects. Monthly mean sediment concentration data of the two stations are compared in-phase and yearly series are analyzed by the method of correlation and regression analysis and causality test. The analysis result shows that, though both of them are located at lower reaches of Manwan and Dachaoshan hydropower stations which are already constructed and in use, the sediment responses of the two stations are different under the regulation of the hydropower stations Annual series at Yunjinghong station are positively correlated but do not match well with those at Chiang Saen station. In addition, the results of Granger causality test on the time series also suggest that the series of maximum monthly mean sediment concentration of the Yunjinghong station each year may give cause for the ones of Chiang Saen station, while the series of minimum monthly mean sediment concentration each year and annual mean sediment concentration of Yunjinghong do not evidently give cause for the ones of the other station. Undoubtedly, this discovery will provide new evidences to assess the impacts of cascades construction in mainstream of the Lancang River on the variation of downstream sediment and its transboundary effects.     

岷江上游干旱河谷区土壤水分含量及其动态

于2002年8月～2003年7月对四川西部理县干旱河谷区土壤水分状况进行了定位研究。结果表明：在理县干旱河谷区，不饲海拔高度0～50cm土层土壤平均含水量总的变化趋势是阴坡比阳坡高。而土壤水分空间异质性阳坡比阴坡大。同一坡向不同海拔的土壤含水量变化为2050m处的最高，1850m处的次之，1450m处再次之，1650m处最少，表明了在干旱区河谷的两岸坡面上部土壤水分状况最好，在坡面下部靠近河流处次之，中下坡水分条件最差。相同海拔高度，不同坡向土壤含水量都表现为随着土层深度的增加土壤含水量增加的趋势，且30～50cm土层的土壤含水量最高。