云南通海盆地的浅层速度结构   总被引：3，自引：3，他引：0       下载免费PDF全文

何正勤  胡刚  鲁来玉  张维  叶太兰  沈坤 《地球物理学报》2013,56(11):3819-3827

为了研究通海盆地的地震动场地效应,在强地面运动的数值模拟计算中需要提供该地区的浅层速度结构模型.为此,在通海盆地开展了10 km高分辨率反射地震勘探和30个测点的面波联合勘探工作.综合本次探测结果与褐煤普查中的电测深和钻孔资料,得到了通海盆地的基岩埋深分布图.结果表明,在通海盆地中部,新生界厚度为100~300 m,整体表现出西南厚东北薄的趋势,盆地沉积层厚度变化明显受到小江断裂南段分支断裂的控制.浅层速度随深度分布表现出在深度相同的情况下,盆地边缘的速度高于盆地中部.  相似文献   

Regulating Environmental Factors of Nutrients Release from Wheat Straw Biochar for Sustainable Agriculture   总被引：1，自引：0，他引：1  

Linin Wei  Gang Xu  Hongbo Shao  Junna Sun  Scott X. Chang 《洁净——土壤、空气、水》2013,41(7):697-701

One mechanism by which biochar application enhances soil nutrient availability is through direct nutrients release from biochar. However, factors controlling the release processes are poorly understood. In this study, the effects of pH, biochar to water ratio, temperature, ionic strength, and equilibration time on the release of PO, NO, NH, K⁺, Na⁺, Ca²⁺, and Mg²⁺ from biochar were evaluated in simulated experiments. The release of PO, K⁺, Ca²⁺, and Mg²⁺ was significantly affected by extraction pH, suggesting that their release from biochar was pH dependent or an H⁺‐consuming process. Correlation analysis indicated that PO and Ca²⁺, PO and Mg²⁺, and Ca²⁺ and Mg²⁺ were co‐solubilized with increasing soil acidity. To a lesser extent, the recovery of the nutrients was also affected by the ratio of biochar to water: more nutrients were soluble with more water supply. In contrast, the release of Na was not affected by pH while the concentration increased with decreasing biochar to water ratio. Meanwhile, other factors (temperature, ionic strength, and equilibration time) had less effect on nutrient release from biochar. Under the influence of pH, the patterns of NO and PO release from biochar were different: extractable NO concentration was not affected by the pH but more PO was released in strongly acidic conditions. Our data suggested that P was mainly retained in inorganic forms while N was in organic forms in biochar. We conclude that environmental factors have marked influences on nutrients release from biochar.  相似文献   

Paleomagnetic data from the Late Carboniferous-Late Permian rocks in eastern Tibet and their implications for tectonic evolution of the northern Qiangtang-Qamdo block   总被引：1，自引：0，他引：1  

CHENG Xin  WU HanNing  DIAO ZongBao  WANG HaiJun  MA Lun  ZHANG XiaoDong  YANG Gang  HONG JingJing  JI WenHua  LI RongShe  CHEN ShouJian  ZHAO ZhenMing 《中国科学:地球科学(英文版)》2013,(7):1209-1220

We report paleomagnetic results from the Late Carboniferous-Late Permian strata in eastern Tibet (China), and aim to clarify the tectonic and paleogeographic evolution of the northern Qiangtang-Qamdo block, which is the key to the study of plate boundary between the Gondwanaland and the Eurasia during the late Paleozoic. Two hundred and nineteen samples-including limestone, muddy siltstone, basalt, lava, and tuff-were collected at 24 sites in the Upper Carboniferous and Middle-Upper Permian successions. A systematic study of rock magnetism and paleomagnetism yields three reliable paleomagnetic pole positions. Both hematite and magnetite occurred in the Late Carboniferous limestone samples. The demagnetization curve shows a characteristic double-component, with the remanent magnetization (ChRM) exhibiting a positive polarity (negative inclination). In the Late Permian limestone, tuff, and basalt, magnetic information were recorded primarily in magnetite, although a small fraction of them was found in hematite in basalt. The demagnetization curve illustrates a double or single component, with the ChRM showing a negative polarity (positive inclination), which has passed the classic fold test successfully. The single polarity features of the ChRM directions of the Late Carboniferous and Middle-Late Permian rocks are respectively related to the Kiaman positive and reversed polarities under the stratigraphic coordinates. This, in turn, indicates that both ChRMs directions represent the original remanence directions. By comparison with the previously published paleomagnetic results from the late Paleozoic rocks in the northern Qiangtang Range, we suggest that: (1) Qamdo and northern Qiangtang block were independent of each other during the Late Carboniferous to the Early Permian periods. The north Lancangjiang ocean basin between the two blocks may have closed before the Middle Permian and been involved in the continent-continent collision stage in the Late Permian-Early Triassic periods. (2) The northern Qiangtang-Qamdo Block paleogeographically was situated at low to intermediate latitudes in the Southern Hemisphere in the Late Carboniferous-Late Permian periods, and began to displace northward in the Early Triassic, with an amount of more than 5000 km northward transport from its current location.  相似文献   

径向基函数算法中插值参数对DEM精度的影响   总被引：2，自引：0，他引：2  

张锦明  游雄  万刚 《武汉大学学报(信息科学版)》2013,38(5):608-612

以多重对数径向基函数插值算法中的插值参数为研究对象,选取了5种不同地貌类型的离散点数据,使用中误差度量指标,研究光滑因子、搜索点数、搜索方向对DEM插值精度的影响,给出插值参数的"最优"取值区间,消除插值参数选择的随意性,更好地指导DEM建模的运用。  相似文献   

数字城市“十分钟健身圈”示范应用系统研究与开发     

陈正富  顾娟  沈刚 《现代测绘》2013,36(4):12-14

数字城市建设既是加快城市现代化的内在要求,也是增强城市综合竞争力的有力工具。天地图各项工作的推进,加快了数字城市的发展,随着全民健身越来越受重视,体育健身信息与基础地理信息相结合的体育信息系统应运而生,本文基于"天地图.江苏"公共服务平台,完成了数字城市"十分钟健身圈"示范应用系统的架构以及系统主要功能的设计,采用B/S与C/S相结合的方式,实现了集电子地图和体育专题数据为一体的"十分钟健身圈"应用示范系统。  相似文献   

山西省层状云飞机云物理观测试验结果分析   总被引：1，自引：0，他引：1  

孙鸿娉  中东东  封秋娟  李义宇  任刚  周学文 《山西气象》2013,(4):35-39,46

利用山西省2008年-2010年64架次云结构的粒子测量系统（DMT）探测资料,配合地面观测和卫星资料统计分析了层状云系的宏微观特征。发现：降水性层状云低云含水量垂直方向上平均为0．03g,m^3,中云含水量垂直方向上平均为0．05g／m30对比分析降水云和非降水云系的微物理特征量,两者存在显著的差异,降水性层状云云粒子有效半径要达到10μm-14μm。对云系不同温度层的微物理特征和云中水分按不同粒子尺度的分配特征进行了对比分析,结果表明：降水性层状云在垂直方向上的微物理结构特征非常明显,也是分层的。高层主要是冰相粒子,主要是冰雪晶,随高度降低冰雪晶的尺度增大,在四个典型温度层的观测中,LWC、云粒子及降水的浓度、尺度相较有很大不同。云中水分按不同粒子尺度的分配可以看出,直径20μm、30μm的粒子含水量较高,对云中液态水含量的贡献较大,降水粒子主要由20μm、30μm的粒子转化。  相似文献   

扇形边界条件下的龙门山壳幔电性结构特征   总被引：10，自引：8，他引：2       下载免费PDF全文

王绪本  罗威  张刚  蔡学林  覃庆炎  罗皓中 《地球物理学报》2013,56(8):2718-2727

沿甘肃碌曲-四川龙门山-重庆合川布设了长周期大地电磁剖面,对龙门山及邻区进行了壳幔电性结构探测,采用更直观合理的扇形边界条件下的反演算法对长周期大地电磁资料进行二维反演.该剖面电性结果揭示了自北西向南东岩石圈深部的若尔盖壳幔高阻块体、松潘壳幔低阻带、龙门山壳幔高阻块体和川中壳幔高阻块体电性结构特征;龙门山逆冲推覆构造带下方的龙门山壳幔高阻体显示为向北西延伸的楔形构造,推断龙门山及松潘-甘孜地块由于受青藏高原东缘和上扬子地块双向挤压,松潘-甘孜地块地壳物质向龙门山逆冲推覆,中下地壳至上地幔向下向南东俯冲,呈现上扬子地块西缘壳幔高阻楔形体插入青藏高原东缘的态势;初步认为上扬子地块西缘深部以松潘壳幔韧性剪切带作为中新生代以来的边界.  相似文献   

国产机载LiDAR安置角误差检校初探   总被引：2，自引：1，他引：1  

成枢  张艳亭  马浩  任国庆  黄刚 《测绘通报》2013,(1):37-40

机载LiDAR的对地定位的误差来源包括单机误差和集成误差.结合试验数据对集成误差中的最大误差源安置角误差检校进行探讨,从安置角误差检校的原理、方法到整个系统精度评定,得出国产机载激光雷达对地定位的相对精度.  相似文献   

面向Android智能移动终端的GIS设计与实现   总被引：2，自引：0，他引：2  

王刚  韩振镖 《测绘通报》2013,(8):77-80

结合"天地图·天津"节点移动端GIS建设情况,分别对Android平台的体系结构、移动GIS架构、移动GIS应用模式、空间数据组织、系统实现及关键性技术等方面进行探讨。  相似文献   

Magnetic detection method for seabed cable in marine engineering surveying     

Bo Yu  Yanchun Liu  Guojun Zhai  Gang Bian  Fumin Xiao 《地球空间信息科学学报》2013,16(3):186-190

The detection and identification of the seabed cable is becoming an important task in the marine engineering. The features of the magnetic anomaly can be used to detect the existence of the seabed cable. The magnetic field model is presented, and the consistency of the magnetic anomaly distribution between the simulation of the model and the observed data is verified. The comparison shows that the seabed cable can be effectively detected and identified with reasonable method.  相似文献