秦淮河水质改善现场调水试验

为了探究不同水闸调度方案对秦淮河水质改善的效果,进行了洪水期、丰水期调度、枯水期调度和降雨初期雨水污染调度等典型时段调水试验。结果表明:通过合理调控闸泵可对秦淮河水质产生积极效果,上游来水、引水的质量和调度时段对于调度效果具有明显影响。     

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.     

渭干河-库车河绿洲生态环境变化特征与防治对策

近50年来，渭干河-库车河三角洲绿洲地区在人类不合理活动的作用下，水与生态环境发生了一系列变化。因此,进行水资源统筹利用规划与管理，统筹兼顾各县的经济发展与生态环境建设对水的需求，以生态系统健康发展为原则，遵循生态规律来进行土地资源的开发利用，开展整个绿洲为单元的生态功能保护与建设是绿洲可持续发展能力的根本途径。     

浅论江南丘陵城市环境特色的传承与发扬——以吉安市中心城市为例

针对当前快速发展的城市化进程中普遍存在的城市特色丧失的状况，阐述城市所处地域环境的唯一性是城市特色构成的关键元素。在归纳我国江南丘陵地带城市普遍具备的自然环境优势，并分析其对城市特色所起的作用后，结合吉安市的具体情况，提出了丘陵地带城市特色的传承与发扬的系列思考，包括城市腹地范围山水特色整体风貌与人文景观遗存的保护和利用；城区外围近郊背景圈中农村居民点规划和产业结构的调整；城区边缘城郊结合部的规划引导；城市片区之间的衔接过渡；城市街区环境特色创造以及具体的城市建设项目的实施等六个层面。     

汾河流域降水量及蒸发量的空间变异性分析研究

借助于地质统计学方法对汾河流域的多年平均降雨量和蒸发量的空间变异性进行了分析,揭示了多年平均降水量和蒸发量的空间变异特征,并应用Kriging方法进行空间插值.分析结果表明,汾河流域多年平均降水量和蒸发量在不同的分割距离范围内有不同的空间相关性,多年平均降水量具有比较明显的地带性,蒸发量分布变化地带性不强.     

湘江长沙段枯水期水位变化及其影响研究

湘江是长沙的母亲河,长沙的发展得利于湘江的恩泽.但近几年来,湘江年年出现特枯水位,特别是2007年以来,长沙站最低水位逼近25.1米的供水警戒线.以湘江2010-2011年度枯水期长沙段水位变化为重点进行分析,并把多年来长沙站出现的最低水位与近几年出现的情况进行比较分析,得出近年来湘江长沙段枯水期的水位变化趋势.最后分析了湘江长沙段枯水期水位走低的各种影响.     

“九龄风度”的内涵与启示

"九龄风度"记载着张九龄历史功绩、刚直气节和政治远见;"九龄风度"的内涵包括才华超群、远见卓识、心系天下安危、为国家尽责、对百姓尽心而笑看生死的风采,以及洒脱豁达、刚直不阿、敢言直谏却淡泊谦让的气度。张九龄以蕴藉、超逸、高雅的文采开山水田园诗文之先河而被推崇为当时的文坛领袖。他超逸、高雅的文学内涵丰富了"九龄风度"。倡议藉"九龄风度"弘扬客家文化,凝聚世界"客家商",促进韶关经济发展。     

新“港口——腹地”文化模型：广西南流江流域文明史的再发现

受群山限制,局促在一种＂马刺型＂（冂）地理区间的南流江水域,历经＂腹地（桂东南）——港口（北部湾）＂间的长期互动,在岭南旧有的＂腹地（西江）——港口（广州）＂文化发展模式之外,营造了独具一格的南流江本土文化。特别是,在南方稻作文化、佛教来华、妈祖入桂、移民实边与民族融合等多方面,南流江流域文明发展史并没有做成＂西江文明史＂的一个附属分支;相反,南流江流域文明史恰好就是＂中华文明多元一体格局＂在岭南地区的深度演绎。目前,它又是构建＂北部湾文化＂必不可缺的有机部件,更是推进广西现代化进程赖以探寻的＂区域文化力＂。     

Sedimentation processes and sedimentary characteristics of tidal bores along the north bank of the Qiantang Estuary

A tidal bore is a unique Earth surface process, characterized by its highly destructive energy, predictable periodicities and magni-tudes, and the production of characteristic sedimentary features. Tidal bores and associated rapid flood flows are highly turbulent flows of the upper-flow regime with a velocity over several meters per second. Reynolds (Re) and Froude (Fr) numbers, respectively, are larger than 104 and 1.0, making them significantly different from regular tidal flows but analogous to turbidity currents. Until now, understanding of tidal-bore depositional processes and products has been limited because of the difficulty and hazards involved with gauging tidal bores directly. The Qiantang bore is known as the largest breaking bore in the world. Field surveys were carried out in May 2010, along the north bank of the Qiantang Estuary to observe the occurrence of peak bores, including regular observations of current, water level and turbidity at the main channel. Several short cores were sampled on the intertidal flats to study the characteristic sedimentary features of tidal bores. Hydrodynamic and sedimentological studies show that the processes of sediment resuspension, transport and deposition are controlled primarily by the tidal bores, and the subsequent abruptly accelerated and decelerated flood flows, which only account for one tenth of each semidiurnal tidal cycle in the estuary. Tidal-bore deposits are generally poorly sorted because of rapid sedimentation after highly mixed suspension by intense turbulence. This behavior is characteristic of the absence of tractive-current depositional components in a C-M diagram. It also goes along with well-developed massive bedding, graded bedding, basal erosion structures, convolute bedding and dewatering structures. Together, these sedimentary features can constitute fingerprinting of turbidites, widely distributed in the deep-water environment. However, a tidal bore is triggered by intensely deformed tidal waves propagating into a shallow-water environment, which returns to regular tidal flows rapidly after the passage of the bore head. The tidal-bore deposits are usually bounded by the intertidal-flat deposits with typical tidal beddings at the top and on both flanks. The difference between tidal-bore deposits (TBD) and tidal sandy/muddy deposits (TSD/TMD) is evident not only in sedimentary structures, but also in the grain-size composition. They can be clearly distinguished in grain-size bivariate plots, typically the plot of mean grain size vs. standard deviation (or sorting). Some trend variations generally exist in mean grain size with TBD>TSD>TMD, sorting with TMD>TBD>TSD (larger value indicating poorer sorting), and both skewness and kurtosis with TSD>TBD>TMD. These findings will undoubtedly shed new light on our understanding of tidal-bore sedimentology, ancient tidal-bore sedimentary facies and environments, and related oil-and-gas field prospecting.     

汾河下游防洪工程施工措施

通过对堤防、控导工程施工中各阶段要点的分析,提出了施工质量过程控制的措施。