黄河中游岩土侵蚀问题及防治对策探讨

黄河中游出露地层岩性主要有古生界奥陶系碳酸盐岩、石炭系和二叠系碎屑岩;中生界三叠系砂泥岩、侏罗系砂泥岩和白垩系砂泥岩;新生界古近系砂泥岩、新近系(原为第三系)红土及第四系风积黄土和现代风积沙。第四系黄土厚度大,结构松散,遇水易解体,具湿陷性,是黄河中游粗泥砂的主要物源;第四系风积沙分布于黄河中游北部,亦是黄河中游粗泥砂的主要物源。岩土侵蚀类型有五:一是风力侵蚀—风沙侵蚀;二是降雨对谷坡面的面状冲刷—坡面侵蚀;三是地表径流对谷底的侧蚀—沟谷侵蚀;四是滑塌对谷坡坡体的破坏—重力侵蚀;五是潜蚀。并对不同侵蚀类型提出了不同的防治对策。     

我国省区间工业结构的异同与结构转换的调控途径

通过计算分析,本文认为我国省区之间工业部门结构既有趋同性,又存在趋异性;趋同性是基本合理的,而趋异性预示着各省区产业结构进一步调整的方向。我国省区工业结构差异主要发现在综合专业化能力、部门深层结构、结构质量三方面。以此为依据,本文提出了我国省区工业结构转换的调控途径。     

PRINCIPLES FOR THE LOCATION OF SYNAGOGUES: SYMBOLISM AND FUNCTIONALISM IN A SPATIAL CONTEXT

Two traditional Jewish approaches to the location of synagogues can be found, one symbolic and one functional. The locational requirements are not identical; the symbolic approach deals with idealistic spatial status while the functional approach poses realistic locational demands. This spatio-locational conflict reflects a problematic situation on both theoretical and practical levels.     

Traffic accessibility and the coupling degree of ecosystem services supply and demand in the middle reaches of the Yangtze River urban agglomeration,China

Journal of Geographical Sciences - The spatial relationships between traffic accessibility and supply and demand (S&D) of ecosystem services (ESs) are essential for the formulation of...     

汉江上游郧县段黄土古土壤序列风化成壤特征以及成壤环境演变

对汉江上游进行野外实地详细调查,在湖北省郧县尚家河台地前沿发现了典型的全新世黄土-古土壤沉积剖面,通过粒度、磁化率、吸湿水和烧失量分析表明,黏粒、细粉砂、磁化率、吸湿水和烧失量在古土壤层S₀出现高值,在L₁、L_t、L₀为低值;而粗粉砂、细砂粒和粗砂粒在S₀为低值,在L₁、L_t、L₀为高值。这些指标的变化说明了全新世以来的气候和成壤环境的变化特征,即在古土壤S₀形成时期,气候温暖湿润,成壤作用非常强烈;黄土堆积时期气候相对干旱,成壤作用较弱。     

人口文化素质与经济发展的互动关系模型研究

根据中国1994～2006年经济发展水平与人口文化素质的统计资料,选取人均GDP和接受过不同教育程度的人口比重分别作为经济发展水平和人口文化素质的衡量指标。经济发展水平与人口文化素质之间的Pearson积差相关分析表明：经济发展水平与人口文化素质之间具有强相关性。针对经济发展水平与人口文化素质之间的强相关关系,运用中国经济发展水平与人口文化素质的时空序列数据,对经济发展水平（y）与人口文化素质（x）进行最优曲线拟合,拟合曲线表明：经济发展水平与人口文化素质之间存在对数关系模型：Y=a＋blnx。     

Regional Variation in Mobility Levels and Timing in the United States

The age patterns of U.S. internal migration, while examined extensively at the national level, have not been fully explored at the regional scale. This study examines, using 1985 - 1990 census data, the state-level variations in two aspects of lifecycle mobility: the mobility level, or the average number of moves made over the lifecycle, and the mobility timing, or the age at which half the lifetime moves are completed. It further delineates typologies of states based upon their age structure of mobility. The study found that regional patterns in the mobility level showed some evidence of the Snowbelt-Sunbelt patterns that characterized economic restructuring in the 1980s. Geographic patterns of mobility timing were less clear; however states in the West and the South showed somewhat more young distributions than the other regions. Further, there was a statistically significant relationship between mobility levels and timing: states with higher mobility levels also exhibited older mobility profiles, as a consequence of disproportionately high elderly mobility rates. The study highlights the regional differences in mobility behavior, and the interplay between the “how much” and the “when” of mobility.     

Fermat猜想的两个等价命题

对每个奇素数p,我们提出了关于p的两个命题:(I)不存在正整数m和n,使代数曲线f(y)=y~3-(2m+1)y-2n的三个零点同时为p方有理整数;(I)不存在正整数m,使不定方程x~2+3y~2=4(2m+1)具有三组正整数解x_i,y_i(i=1,2,3),满足x_1=x_2+x_3,x_1~2+x_2~2+x_3~2=6(2m+1)。本文旨在证明(I)及(I)都与关于素数p的Fermat猜想等价。     

Fault structures and their geoelectric parameters in the epicentral zone of the 27 September 2003 Chuya earthquake (Gorny Altai) from resistivity data

This paper presents an integrated measurement technique based on DC methods (vertical electrical sounding, electrical resistivity tomography) which was used to identify faults and determine their geoelectric parameters in the western part of the Chuya basin. New information on the structure of the Chagan River valley located in the zone of the disastrous 27 September 2003 Chuya earthquake has been obtained from the results of these methods. Geoelectric cross-sections of the sedimentary sequence and the upper part of the basement were obtained from VES data, showing the block structure of the study area. Electrical resistivity tomography sections confirm the presence of a major fault between basement blocks of different heights and indicate the presence of faults bounding the valley on its right side and in the southwestern part.