区域自然灾害系统基本单元研究-Ⅱ:应用部分——湖南省综合农业灾情区域分异规律

本文应用灾害系统基本单元理论,以湖南省农业自然灾害为例,在地理信息系统支持下,将湖南省农业自然灾害系统划分为３２５２４个基本单元。进而,以民政部１９７８～１９９３年农业灾情统计数据为标准,通过多因子逐步回归的方法,建立了反映湖南省多年平均状况的五种主要农业灾害灾情模型。最后,以灾害基本单元为最小空间分异单位,对综合农业灾情分异规律进行了探讨,并首次提出了基于自然单元的湖南省综合农业灾情的分异规律首先是受地势控制的东西分异的主要结论。     

放射性同位素自动分装系统

研制的ＴＦ—Ａ 设备是用计算机控制的同位素自动分装系统。它由分装防护箱、机械传动、计算机自动分装和辐射剂量监测部分组成,可使γ辐射强度减弱９０％ 以上,并可隔室操作,以确保工作人员的安全和健康     

近五年中国自然灾害空间分布格局及其月动态变化研究

作者根据《中国减灾》所载１９９０～１９９４年月灾情记录，经统一编码和标准化处理，建立了以行政县为基本单元的数据库。进而对近五年来中国自然灾害空间分布及其月动态变化进行分析，并与１９４９～１９９０年中国自然灾害的平均状况进行对比。     

煤矿区采煤沉陷灾害分析与对策研究

煤矿区采煤沉陷问题,目前已引起世界各产煤国的普遍重视。我国因农村人口稠密,所以采煤沉陷的危害更为严重。本文全面系统地分析了采煤沉陷在地表可能造成的各种危害,并以减轻危害程度为目标,提出了开采前和开采过程中的预防措施,以及采后地面沉陷的治理措施。     

栽种沙枣以改善黄河三角洲地区生态环境

胜利油田位于我国黄河三角洲地区，潜水位高，水的矿化度大。生态环境恶劣，对植物尤其对木本植物的生长不利，整个地区生长的多是抗盐碱能力强的草本植物。针对油田的特殊环境条件，综合有关资料，介绍了以沙枣为代表的植物特性，特别强调了其抗盐碱、降低土壤矿化度和潜水位、增加土壤有机质和引起植被变化的特性。指出黄河三角洲也有些土质较好的、适于作物和木本植物生长的地区，改良盐碱地可以以这些地区为基点，放射性地向外逐步试验沙枣的种植，以探索改善生态环境的途径。努力做到边发展经济，边改善环境，达到经济效益、社会效益和环境效益三统一。     

浙江仇山矿区膨润土、高岭土矿石矿物地质特征

仇山膨润土矿赋存于上株罗统劳村组火山岩中，I、Ⅱ矿层为主矿层，成矿母岩为火山玻璃岩。矿石经X衍射，差热及阳离子交换量等手段测试，按其埋藏深度由浅而深依次为钙基膨润土→钠钙基膨润土→钠基膨润土→高岭土，具蒙脱石向高岭石矿物变化的地质特征。对其形成的成因机理作了分析探讨，系不同的成矿方式和介质条件所致。     

广西来宾栖霞组缺氧沉积环境地球化学特征

地层的岩石地球化学特征是判断其形成环境氧化还原条件的重要手段之一。本文对广西来宾铁桥剖面栖霞组中层纹状灰岩和含泥质灰岩进行地球化学分析 ,结合栖霞组沉积学和古生态学特征 ,对栖霞组沉积环境进行了探讨。岩石微量元素含量、黄铁矿矿化程度 (DOP值 )、痕量元素V/Cr、Ni/Co、U/Th、V/(V +Ni)等比值的研究结果显示 ,研究区具有缺氧沉积成因的地球化学特征。     

珠江口水环境可持续发展的探讨

大量悬浮物的输入、水质污染和咸水入侵 ,严重威胁珠江口水环境的可持续发展。在信息革命技术支持下 ,应该根据珠江口的环境现状 ,充分利用先进的生产技术和管理方法 ,通过建立和完善珠江口海洋环境立体监测系统 ,加强环境的先期审查工作 ,建立有效的环境管理体制 ,将市场、政府和个人结合在一起 ,制订出可行的发展战略 ,以实现珠江口水环境的可持续发展     

Anthropogenic Calcium Particles Observed in Beijing and Qingdao, China

Analysis of individual particles collected at Beijing in northern China revealed that particles abundant in calcium (Ca) always constituted a large fraction of mineral particles in the urban atmosphere. The particles were characterized by cubic morphologies. The major mineral element in the particles was Ca and few or no other mineral elements were detected. A large number of the particles were in the range of diameter <1 μm, where common natural mineral particles were rarely detected. The contribution of the Ca particles to the volume of total mineral particles greatly exceeded that of other mineral particles during non-dust-storm periods and was comparable to that during dust-storm periods. Reagent film tests showed that particulate sulfate and nitrate formation on the Ca particles was similar to that on common mineral particles. These results indicate that a large portion of Ca in the atmospheric particulate matter in Beijing was from anthropogenic sources rather than from natural sources, and the anthropogenic Ca particles acted as a significant medium for the formation of sulfate and nitrate. Similar particles were also detected at Qingdao, a coastal city in northern China. Data of a dust storm event showed that Ca-abundant particles from East China arrived there and moved out of the continent, similarly to Asian dust storm particles, suggesting possible contributions of anthropogenic Ca even in Asian dust storm samples in the downstream areas. Therefore, Ca may not be a good indicator of Asian dust from natural sources. However, the Ca particles, due to their unique shapes and elemental compositions, may provide an indicator for the atmospheric dispersion of anthropogenic particulate matters in East Asia.     

Climatic and Environmental Changes in the Source Areas of Dust Storms in Xinjiang, China, during the Last 50 Years

The desert environmental changes in the source areas of dust storms occurring in Xinjiang are discussed based on the climate changes and the impacts of human activities in Xinjiang during the past 50 years. The results show that the climate in Xinjiang is changing from a warm-dry type to a warm-wet one. The warm-wet climate has been obvious since the mid-1970's, and especially the sensitivity of the regional climate change in this arid area is obviously revealed by many factors, such as the characteristics of the local climate change in south Xinjiang and north Xinjiang, the difference of climate change in the alpine zones and the basins, and the change of areas of the waters bodies. Furthermore, these factors also reveal the difference in the regional climate change between Xinjiang and central and eastern areas of China. The occurrence and development of dust storms are directly affected by the precipitation, air humidity, status of underlying surface, etc. in the arid areas. The frequency and intensity of dust storms are closely related to the natural conditions, changes of climate and desert environment, as well as the dynamic conditions (i.e., weather systems) in the source areas of dust storms. Therefore, global warming is one of the main causes resulting in the degradation of the ecological environment and the frequent occurrence of natural disasters, especially the disasters of sand drift and dust storms in the arid areas since the late-1980's, which reveals that the inland arid areas are sensitive regions to climate changes.