存量批地空间数据清理、整合技术方法——以安仁县为例

为解决湖南省建设用地审批红线空间数据问题,保障新增建设项目顺利上报审批,并支撑湖南省建设用地批后监管业务,研究建设用地审批红线空间数据清理、核查、整合处理的技术方法,并以安仁县为例进行验证。经试验,结合研究的技术方法解决了安仁县2009—2019年形成的批地问题图斑的问题,在全省范围可推广。     

蒙城地震台地磁Z分量日变化特征分析

利用蒙城地震台近20年的地磁Z分量观测资料,对磁静日幅度、磁扰日幅度和磁静日低点时间的年变化与长期变化进行了分析,结果表明,Z分量日变化特征明显。由此总结出Z分量变化的一些基本特征,对识别地磁场异常变化或干扰变化具有一定的参考价值。     

A Review of Mineral Resources and GIS Applications in Mineral Resource Assessment in Northeast China

IntroductionThe Northeast China region locates in the centre of Northeast Asia economic zone, and borders onRepublic of Mongolia in the north, Russian Far Eastin the east, and Democratic People, s Republic ofKorea in the south. It includes three provinces…     

Study of red tide prediction model for the Changjiang Estuary

ＩＮＴＲＯＤＵＣＴＩＯＮＡｑｕｉｃｕｌｔｕｒｅａｒｅａｒｅｄｔｉｄｅｓｉｇｎａｌｓｏｃｅａｎｐｏｌｌｕｔｉｏｎａｎｄｄｉｓａｓｔｅｒ.Ａｌｔｈｏｕｇｈｅｎｖｉｒｏｎｍｅｎｔｓｃｉｅｎｔｉｓｔｓｈａｖｅｃｏｎｄｕｃｔｅｄｍａｎｙｉｎ ｄｅｐｔｈｒｅｓｅａｒｃｈｅｓｏｎｔｈｅｃａｕｓｅａｎｄｆｏｒｍａｔｉｏｎｍｅｃｈａｎｉｓｍｏｆｒｅｄｔｉｄｅ ,ｍａｎｙｏｆｉｔｓａｓｐｅｃｔｓａｒｅｓｔｉｌｌｕｎｋｎｏｗｎｂｅｃａｕｓｅｒｅｄｔｉｄｅｉｓａｃｏｍｐｌｅｘｐｈｅｎｏｍｅｎｏｎａｎｄｔｈｅｅｃｏｌｏｇｉｃ…     

Study on transmission mechanism of thermal infrared remote sensing for abrupt geothermal anomaly in volcanic region

Ｇｅｏｔｈｅｒｍａｌａｎｏｍａｌｙｉｓａｐｈｅｎｏｍｅｎｏｎｔｈａｔｕｎｄｅｒｇｒｏｕｎｄｔｅｍｐｅｒａｔｕｒｅａｎｄｇｅｏｔｈｅｒｍａｌｇｒａｄｉｅｎｔｉｎｃｒｅａｓｅｓｍｕｃｈｍｏｒｅｉｎｔｈｅａｒｅａｔｈａｎｉｔｓｓｕｒｒｏｕｎｄｉｎｇｓ（Ｘｉａ,１９７９）．Ａｂｒｕｐｔｇｅｏｔｈｅｒｍａｌａｎｏｍａｌｙｍｅａｎｓｔｈａｔｕｎｄｅｒｇｒｏｕｎｄｔｅｍｐｅｒａｔｕｒｅｏｎｓｏｍｅｓｐｏｔｓａｓｗｅｌｌａｓｔｈｅａｆｆｅｃｔｅｄｔｅｍｐｅｒａｔｕｒｅｏｆｓｕｒｒｏｕｎｄｉｎｇａｒｅａａｂｒ…     

Triploidy induction with heat shocks toPenaeus chinensis and their effects on gonad development

Heat shocks effectively produced triploids inPenaeus chinensis. Fertilized eggs heat shocked (28–32°C) for 8 to 16 minutes, starting from 8 to 20 minutes after spawning, resulted in triploidy induction rates of 39%–75%. Several triploid populations were cultured to 10 cm. In a triploid population, two kinds of ovaries were observed. Histological examination showed apparent differences between these two kinds of ovaries, whereas among male shrimp, there were no such differences. Contribution No. 3465 from the Institute of Oceanology. Chinese Academy of Sciences. The study was supported by the International Foundation for Science, Asian Fisheries Society and Chinese Climbing Project PDB 6–2, and Chinese National 863 Project (No. 863-819-01-05).     

浙东南地区蜡石矿及其成矿远景

本文总结了浙东南地区蜡石矿的分布,成因类型及其特征;成矿地质条件和控矿因素;划分了成矿远景区和提出了地质工作布置建议。     

人工神经网络在云南5月雨量预测中的应用

提出了一个基于３层ＰＢ神经网络的云南５月雨量的短期气候预测模型。由于神经网络本身是一个非线性动态系统,将其应用到短期气候变化预测这一非线性系统中,更能反映出气候系统状态量之间的物理关系和动力行为特性。并用该预测模型对云南５个区域１９９１～１９９８年的５月雨量距平趋势进行了共４０次的预测试验和检验,其预测的距平符号相关准确率可达到７７．５％。     

基于多元时间序列的Kn近邻预测模型

提出了一种基于多元时间序列的Ｋｎ近邻短期气候预测模型。该模型既保留了Ｋｎ近邻算法的优良特性,同时又考虑了气候系统有关状态量之间的物理关系和动力行为特性。用该模型对云南各区域的平均月雨量距平值进行预测试验,其对云南１９９１年５月～１９９８年６月的月雨量距平值预测检验的距平符号相关准确率为６３．５％,对云南１９９１～１９９８年的５月雨量距平值预测检验的距平符号相关准确率则可达到７０．０％。该模型的建立具有一定的实际业务应用价值。     

Lithospheric thermal and compositional structure of South China jointly inverted from multiple geophysical observations

The detailed lithospheric structure of South China is the basis for the understanding of tectonic processes of eastern China.Specifically,two essential issues in the study of lithospheric structure are the thermal and compositional structures,which are usually derived from either geophysical or geochemical observations.However,inversions from single geophysical or geochemical datasets have certain limitations,making it necessary to develop joint inversions of geophysical,geochemical and petrological datasets.In this paper,through thermodynamic simulation and probabilistic inversion,we inverted multiple datasets including topography,geoid height,surface heat flow and surface wave dispersion curves for the 3D lithospheric thermal and compositional structure of South China.The results reveal a thin(<100 km)and flat LAB beneath the South China Fold System Block and the lower Yangtze Craton.Also,we found that the lithospheric mantle is primarily composed of saturated peridotite,indicating that the ancient refractory lithospheric mantle has been replaced by new materials.The dominant dynamic mechanism for lithospheric thinning in eastern South China may be the flat subduction of ancient Pacific slab,while thermal erosion may have also played a significant role.In contrast,the LAB depth beneath the Sichuan Basin is much thicker(>200 km),suggesting that the thick and cold craton lithospheric roots are retained.There may exist a discontinuous interface beneath the Sichuan Basin,with the saturated lower layer thicker than the refractory upper layer.As a result,the lithospheric mantle of the Sichuan Basin and surrounding regions is mainly composed of saturated and transitional peridotite.