基于GIS与Geo-CA模型的半干旱区土壤盐碱化动态模拟研究

土壤盐碱化是半干旱地区土壤退化的重要表现形式之一,其发生发展是一个复杂的非线性动力学过程.利用地理元胞自动机对复杂系统时空动态演化过程具有较强的计算与模拟能力的特点,以吉林省西部盐碱化土地为研究区,在GIS的支持下系统分析了土壤盐碱化的特征及其影响因子,建立了基于Geo-CA的土壤盐碱化动态模型,模拟了吉林省西部土地盐碱化发生发展的时空动态规律.     

山西省地表水水功能区划分及其管理

水功能区的划分是实现水资源综合开发、合理利用、积极保护、科学管理的基础工作。根据“全国水功能区划技术细则”，结合对山西省黄河流域的自然、社会情况，尤其是水资源状况的综合分析，系统介绍了水功能区划的方法，对山西省黄河流域河流地表水进行了水功能区划并提出管理建议。     

实现山西机电产品进出口可持续发展的对策研究

针对山西省机电产品进出口的现状与存在问题，提出了实现山西机电产品进出口可持续发展的对策。     

山西省科技创新体系建设简述

总结了近年来山西省在科技创新体系建设方面取得的成就和存在的问题，提出了今后建设山西科技创新体系的指导思想和战略模式以及山西科技创新系统的目标体系，并对山西科技创新体系的建设提出了一些建议。     

吉林珲春新近系土门子组孢粉组合及其意义

通过对吉林珲春土门子组孢粉样品分析。建立了Quercoidites-Ulmipollenites-Liquidambar-pollenites组合。根据孢粉植物群特征及其与周围地区对比，其地质时代归属新近纪中中新世为宜。孢粉组合中喜温成分占多数，亚热带成分如Caryapollenites、Liquidambarpollenites等也较为常见，反映了当时比较温暖湿润的暖温带-亚热带气候，在我国第三纪植物群区系中属于东部落叶阔叶林植物区。     

安徽省中小学学校体育发展探析

运用文献资料法、专家访谈法、问卷调查法、数理统计法等,在对安徽省中小学学校体育现状进行调查的基础上,通过分析研究,提出安徽省中小学学校体育发展的具体战略措施,为省教育主管部门宏观决策提供依据.     

Stratigraphic implications of Sinian-Early Cambrian volcanic ash beds on the Yangtze Platform

Volcanic ash beds from shallow- to deep-water facies strata of the Sinian-Early Cambrian (Meishucunian) on the Yangtze Platform consist of bentonites and tuffites which are readily recognized in the field by their physical features and confirmed by geochemical analyses.Geochemistry suggests that the volcanic ash beds in Meishucunian time are rhyolite and rhyodacite while those in the Qiongzhusian and Sinian are andesite and trachyandesite.The ash beds in the time-equivalent strata, even in different areas display rather similar geochemical features, whereas the ash beds in different strata even in the same areas show large chemical difference.The results suggest that these ash beds can be used for intra- and extra-basinal correlations of the Sinian-Early Cambrian interval on the Yangtze Platform.Additionally, these ash beds suggest high potentials for further U-Pb dating strategies.     

NPP distribution related to the terrains along the North-South Transect of Eastern China

Vegetation net primary productivity (NPP) is defined as the accumulative amount of organic matters per unit area and time, which is calculated from the difference between accumulative photosynthesis and accumulative autotrophic respiration by green plants. Since the NPP reflects the physiological and ecological characteristics of the plants and the interactive results of the environmental factors, it is an important index to evaluate a structure of ecological system, functional features and …     

Simulation of meridional overturning in the upper layer of the South China Sea with an idealized bottom topography

The South China Sea (SCS) is the largest marginal sea in the northwestern Pacific. Several important water gateways exist around the SCS, such as Luzon Strait, Taiwan Strait, etc., that lie in the northeastern SCS, and others like Kalimantan Strait, Balawan Strait, etc., lie in the south. Luzon Strait connects the SCS and Pacific via the Philippine Sea, and its water exchange has significant impact on the interior circulations of the SCS[1]. Since direct observation data about the …     

Deep-water Earliest Oligocene Glacial Maximum （EOGM） in South Atlantic

The most prominent cooling event of the Earth surface during Cenozoic in the long-term transition from a non-glaciated planet, or “green-house world”, to a polar, glaciated planet, or “ice-house world”, is the Earliest Oligocene Glacial Maximum (EOGM) above the Eocene/Oligocene boundary at about 33.7 Ma. Planktonic and benthic foraminiferal oxygen and carbon isotopes, carbonate content, and coarse fraction, along with high-resolution color reflectance and magnetic susceptibility records during 35-30 Ma, from deep-water Sites 1262 and 1265, Ocean Drilling Program (ODP) Leg 208 in South Atlantic, reveal the global cooling event occurring in both surface and deep oceans. The results show that the earliest Oligocene δ^18O values during 33.5-33.1 Ma represent the magnitude of continental ice sheets on east Antarctica and indicate the large decrease in both surface and deep water temperatures of worldwideoceans. The δ^13C records show the large excursion during the period of EOGM event and indicate some types of shift in global carbon reservoir, probably demonstrating the sudden increase in organic carbon burial rates and the changes in the distribution and timing of production. At the same time, lithologic composition, carbonate content, color reflectance, and coarse fraction brought about significant changes close to the Eocene/Oligocene boundary, reflecting the abrupt deepening in the carbonate compensation depth (CCD). Changes in carbonate content were revealed from the color reflectance identify periodicities associated with eccentricity of the Earth‘s orbit (100 and 400 ka), further indicating orbitally forced global climate variations in the Early Oligocene.