江汉平原北部明清时期的环境演变

通过对江汉平原北部蔡垱西剖面沉积物粒度、地球化学元素、孢粉等相关数据的综合分析,揭示了该地区约1250年以来环境演变历史。通过沉积物的野外观察、粒度数据分析及剖面所处地貌部位的综合分析认为,该剖面沉积物主要为汉江等周围水系洪水带来的泥沙泛滥至低洼平原区,并以近乎停滞的低缓流速沉积而成,所以沉积物以细粒的黏土质粉砂为主,...     

Evolution of an Eocene-Oligocene Saline Lake Depositional System and Its Controlling Factors,Jianghan Basin,China

The Upper Eocene–Lower Oligocene Qianjiang Formation of the Jianghan Basin in central China consists of a 4 700-m-thick lacustrine succession, containing 1 800 m of halite deposits. The maximum thickne...     

江汉湖群气候效应研究

以洪湖为例，分析了江汉湖群湖泊对气温、降水的影响，还分析了围湖造田对湖区降水的影响．     

江汉平原耕地变化的经济损失分析

对江汉平原2000～2003年耕地流失的基本态势及其经济损失进行定量分析,为缓解耕地流失形势、确定耕地流失的经济补偿提供决策依据.估算表明,2000～2003年江汉平原耕地资源净减少28 968.69hm2,耕地流失所带来的经济损失达82.07亿元,年均损失20.52亿元.其中,耕地资源的市场价值损失72.61亿元,占88.47%;目前无法通过市场价格机制体现的非市场价值流失9.46亿元,占11.53%.耕地流失经济损失的货币化计量,是有效解决农地生态补偿机制构建的一个技术难题,为确定农地生态补偿标准、规范人类活动的性质和干扰程度、限制土地的过度开发和优化农地景观格局提供决策依据.图1,表6,参14.     

The agricultural assessment of climatic resource and modeling in Jianghan plain-lake district

The feature of the climatic resource and the agricultural assessment in Jianghan plain-lake district are discussed. In order to exploit the climatic resource, we have recommended some three dimensional agriculture development models in this region according to the types of land use, such as paddy field ecological zone, dry land ecological zone, outskirts ecological zone of the city, waterbody ecological zone, woodland ecological zone. Foundation item: Supported by the National Natural Science Foundation of China (49871071), Key Items of Agricultural Exploration of HuBei Province and Chinese Academy of Sciences (962T0507, KN95-03) Biography: Wang Xue-lei (1965-), male, Associate professor. Research direction: wetland ecology.     

三峡工程的防洪效益与江汉平原产业结构调整设想

江汉平原一直遭受洪水的威胁,三峡工程的修建将大大减少洪水可能带来的直接和间接经济损失。为此,我们提出江汉平原产业结构调整的设想：１）增加农业基础设施投资,发展高效农业;２）培育和建设医药化工、机械电子、食品饮料、纺织服装、建筑建材等支柱产业;３）大力发展第三产业;４）开发地下矿产资源兴建以盐化工为主的化工企业;５）适当发展能耗大的工业。     

江汉平原生态系统服务价值变化解析

以湖北省江汉平原为例,采用基于专家知识的AHP方法、LMDI分解模型等重点考察该区域土地利用特征及生态系统服务价值变化的影响因素分解问题。研究结果表明:(1)1995年以来该地区耕地、林地、草地和自然保留地面积减少,水域和建设用地面积增加,以耕地和水域为主的用地结构变化相对平稳;(2)采用基于专家知识的AHP方法确定不同时期的价值密度修正系数,发现各地类修正系数均以2007年为基准呈现随时间增长的趋势;(3)利用改进的生态服务价值计算方法,发现各地类生态服务价值均有所增加,不同时期各地类价值贡献基本呈现耕地、水域最多,林地、自然保留地次之,建设用地与草地最少的特征;(4)利用LMDI模型考察生态服务价值变化的分解效应,研究显示人口增加、土地结构变化与价值密度提高具有增值效应,对价值变化的效应比重分别为13.12%、9.23%、90.70%;人均土地面积降低对价值变化具有减量效应,所占比重为-13.06%,在一定程度上抵消了三类因素的增值效应。     

微分反馈控制与延迟微分反馈控制

证明了微分反馈控制洛伦兹系统在三个平衡点S0，S1和S2的可控性，提出了延迟微分反馈控制DDFC，DDFC利用可测变量的微商进行反馈，理论证明DDFC加于洛伦兹系统的第3个方程时3个平衡点均不稳定可控，而加于洛伦兹系统的第2个方程时平衡点S0不可控而平衡点Sl和S2稳定可控，用Matlab进行数值仿真，调节延迟时间τ和控制增益k，DDFC系统能自动寻找和稳定不同的不稳定周期轨道UPO，实现混沌控制。     

Magnetism parameters characteristics of drilling deposits in Jianghan Plain and indication for forming of the Yangtze River Three Gorges

The forming time of the Yangtze River Three Gorges is considered as one of keys in the research on the Yangtze River, also is one of the most disputed hotspots. In order to solve the difficult problem, the authors adopt the internationally recognized thoughts and methods of substance tracing from source to sink. The lithologic characteristics, magnetic parameters and magnetic mineral characteristics of deposits in 2 bores are analyzed, which are both sampled from the sedimentary center of the Jianghan Plain. The results are as follows： At about 110 m depth of the core, the contents of coarse materials and stable magnetic mineral both increase significantly. Meanwhile, the magnetic susceptibility of sediment, saturation isothermal remanent magnetization and magnetic susceptibility values of anhysteretic remanent magnetism increase suddenly, which all reflect that at about 110 m depth, the important adjustment has appeared in water system of the Jianghan Plain, and the sedimentary environment and material composition have changed greatly. And it may be the horizon where the Yangtze River Three Gorges formed, its forming time reflected by the paleomagnetic dating is between 1.17 and 1.12Ma B.P.