Monitoring the sandstorm during spring season 2002 and desertification in northern China using SSM/I data and Getis statistics

A massive sandstorm enveloped most part of northern China during the spring season 2002. Monitoring the evolution of sandstorm and desertification has become one of the most serious problems for China's environment. Since 1989, one of the most advanced and operational passive microwave sensors is the DMSP SSM/I (special sensor microwave imager) operated at seven channels (19, 37, 85 GHz with the vertical and horizontal polarization and 22 GHz with vertical polarization only). In this paper, the sandstorm and desertification indexes, SDI and DI, are derived from the radiative transfer equation, and are employed with multi-channel measurements of the DMSP SSM/I for monitoring the sandstorm and desertification in northern China. Some SSM/I data in 1997 and 2001 are employed. The algorithm of Getis statistics is developed to categorize the spatial correlation and its evolution these days. It is demonstrated that the SSM/I indexes, SDI and DI, and its Getis statistics are well applicable for monitoring the sandstorm and desertification.     

浅谈人工挖孔桩

分析了人工挖孔桩施工中遇到的问题(如水、溶洞、淤泥层、流砂),并提出了相应的处理措施。     

岩溶地区100 m深钻孔桩施工技术——以眼镜塘特大桥为例

结合眼镜塘特大桥超长钻孔桩施工以及岩溶地区的地质状况,根据现场施工管理经验,介绍了客运专线岩溶地区100m深钻孔桩施工技术,提出了冲击法钻孔、深层溶洞处理、塌孔以及沉碴清除的一些控制措施。     

长春市双阳吊水壶风景区的岩溶洞穴群

在阐述长春市南部双阳区吊水壶岩溶洞穴群特征的基础上,进一步对该区发育岩溶洞穴群的地质环境、成因和形成时代进行了探讨。     

贵州喀斯特地区生态经济类型划分

根据生态经济学理论,采用主成分分析法和聚类分析法,选取 47个指标对贵州 75个喀斯特县(市)进行生态经济类型划分研究,将 75个喀斯特县(市)分为 2个一级类型、9个二级类型、18个三级类型、8个四级类型,并对不同类型的发展潜力在命名上作了定位,为进一步研究不同生态经济类型的发展提供了基础。     

喀斯特地区的枯水资源承载力研究

在结合前人对水资源承载力研究的基础上,考虑到不同时段水资源差异和喀斯特地区枯水资源的特殊性,给出了喀斯特地区枯水资源承载力的概念。并针对喀斯特地区枯水的特点,分析了影响枯水资源承载力的枯水资源条件、生态环境、社会生产活动及经济技术水平等因素。同时提出相应的提高枯水资源承载力的措施。     

浅谈太原地区石质荒山造林绿化的要点

通过对太原地区石质荒山立地条件的分析，提出了适宜石质荒山造林的5项技术措施。即适树省水、整地蓄水、保根带水、选天时抓水、栽植保水。     

泰安岩溶水系统地下水动力环境演化规律研究

从地下水水位的时空演化、地下水水位降落漏斗的形成和演化、地下水埋藏条件的演化以及地下水流场的变异等方面，分析总结出泰安岩溶水系统地下水动力环境的演化规律；指出岩溶水系统地下水动力环境演化是人类活动的结果。     

Contributions of different land cover types in Otindag Sandy Land and Bashang area of Hebei Province to the material source of sand stormy weather in Beijing

Different land cover types in Otindag Sandy Land and Bashang area of Hebei Province are linked to a material source of sand stormy weather in Beijing based on results of field vegetation and soil survey and laboratory works. Results of grain size analysis show that dust release potential in per unit area of moving sandy land is small,while lowland meadow and meadow steppe in stony hills have high potential of releasing dusts in per unit area during sand stormy weather occurrence. Further considering the effects of vegetation, it is inferred that the moving sandy land served as a material source of past dust storm and the possibility of dust release in per unit area is low in current time.Typical steppe in stony hills is undergoing desertification and its dust release possibility in per unit area is high. Farmland has strong potential of release dusts when they are ploughed in spring, but a large amount of therophytes grow and thus prevent dusts from release when cultivation was terminated.Potentials of dust release in per unit area in fixed sand dunes,stony mountain meadow steppe and low land meadow are lowdue to high cover of perennials. Sand dune reactivation and desiccation of lakes and lowlands under estimated future climatic change will make them serve as a future material source of sand stormy weather.     

岚皋大巴山岩溶地貌

认为岚皋大巴山岩溶地貌发育在寒武系石灰岩地层的高夷平面上，由于受岩性、地质构造、地貌和气候等自然条件的影响，地表、地下岩溶地貌发育不够均匀，但以溶洼丘峰为主，溶洼往往积水成湖，是我国南北方典型岩溶地貌的过渡类型区。