广东封开河儿口盆地的古地理环境初探

渔涝河的上游干流—七星河长 4 2km ,在中更新世中期至晚期形成。峒中岩、黄岩洞和罗沙岩等洞穴的动物群化石测龄 14 8～ 2 2 4kaBP ,时间跨度约 13万a而该化石堆积层的厚度仅 1m余 ,且与七星河的第一级阶地类高 ,反映晚更新世早期至中期该盆地底部的构造升降基本上稳定。这是同期广东许多河谷地段没有构造抬升的一个重要信息 ,而且可将今日广东第一阶地沉积的最老年龄从目前已知的 5 1 9kaBP推延伸到 15 0kaBP。     

Correlation of coral fluorescence with nearshore rainfall and runoff in Hainan Island, South China Sea

Under UV-laser excitation, the Porites coral from Longwan bay waters. Hainan Island, could emit yellow-green fluorescence. After fitting the data of the fluorescent intensity (FI) of the coral with the rainfall (RF) in nearshore area of Qionghai. a good relationship between FI and RF was found with a linear formula of RF = 889 — 4.54 FI and a correlation coefficient of 0.78. Based on this formula, the rainfall sequence from 1982 to 1997 has been reconstructed. The peak annual rainfall is usually related to global El nino events. By fitting the data of the fluorescent intensity and the runoff (RO). a quadric formula was obtained as RO = — 0.0279FI —18.59 FI - 950.9 with a correlation coefficient of 0.74. The reconstructed runoff sequence from 1982 to 1997 coincided with the rainfall occurrence. The results indicate that flood and drought incidents in coastal areas of the south China are affected by global change to a great extent.     

闽江下游白岩潭潮位站洪水位研究

白岩潭潮位站位于闽江下游感潮河段，其水流受到上游来水与口外潮汐的共同作用。文中探讨了洪水期间白岩漂水位的数值计算法、相关分析法和组合概率法，对各自的长处与存在的问题进行了分析。所得结论对感潮河道的洪水位研究具有一定的指导意义。     

中小型河道纳污能力计算方法研究

在对河段污染源进行概化的基础上提出纳污能力的计算方法及计算公式。结合水资源保护的实际需要，给出不同功能区组合情况下的纳污能力的计算方法，为水资源保护与规划提供了一种简捷有效的方法。     

氯苯类在地面水中的光降解研究

本文报道氯苯和邻二氯苯在地面水中的光降解作用(动力学参数、量子产率等)以及影响光降解作用的因素,并讨论了光降解机理。     

和田河流域生态脆弱性成因辨识

通过献资料和野外考察,认为和田河流域的脆弱生态环境是长期的自然作用过程及人类活动干预下形成的。自然地理要素有脆弱性的一面,不合理的人类活动加剧了生态环境退化的进程。和田河流域脆弱生态环境是水、植被环境恶化导致的生态平衡失调形成的。总体表现为以荒漠化为主体的环境问题日益加剧,并通过土地沙漠化、土壤盐渍化、草场退化、生物多样性丧失,以及干旱、风沙、盐碱、洪灾等表现出来。综合评价结果表明,和田河流域的生态环境质量属中等脆弱。     

REE geochemistry of suspended sediments from the rivers around the Yellow Sea and provenance indicators

Rare earth element (REE) compositions of the suspended sediments from the rivers around the Yellow Sea were different in that Korean river sediments (Han, Keum and Yeongsan Rivers) yield stronger fractionations than Chinese river sediments (Changjiang, Huanghe and Yalujiang), shown by obvious enrichments of LREE (light rare earth element) relative to UCC (upper continental crust).Variations of source rock compositions in the drainage basins are responsible for the differences of REE compositions between the river sediments. REE fractionation parameters including (La/Yb)ucc and (Gd/Yb)ucc as well as the ratios of La/Sc and Th/Sc can be treated as proper proxies for identifying the Chinese river sediments from those Korean river matters, and furthermore, for studying the provenances and paleoenvironmental changes of the marginal seas of China.     

山西省河道工程管理浅议

介绍了山西省河道工程管理的现状,分析了河道管理体制工作中存在的问题,探讨了山西省河道工程管理发展方向及搞好工程管理应采取的措施。     

论三代前黄河下游河道的大致走向

黄河下游河道的走向，历来是史家争议之焦点。但史家关于三代前下游河道的研究却少之又少．所以本文从记载黄河下游河道的古今文献、考古资料等，勾勒出历史时期黄河下游的河道应在今日山东地区。