季节偏差纠正下的遥感AOD产品降尺度BGIM算法     

梁玉  邹滨  冯徽徽  刘宁 《遥感学报》2022,26(8):1602-1613

MODIS 3 km DT（Dark Target）卫星气溶胶光学厚度AOD（Aerosol Optical Depth）数据产品已广泛应用于大气污染监测,但受反演方法限制,该数据产品像元缺失严重、时空覆盖度低、精度偏低。相比,MODIS 10 km DT_DB_Combined AOD数据产品因融合DT和DB（Deep Blue）两种反演算法,一定程度上可弥补MODIS 3 km DT AOD数据产品在时空覆盖度与精度方面的缺陷,但分辨率偏低。此外,受气溶胶组分来源的季节变化与地表反射率估算的季节性误差影响,MODIS AOD数据产品精度同时也存在季节性特征。本文由此以京津冀为试验区,顾及AOD季节变化特性,开展MODIS 10 km DT_DB_Combined AOD数据产品偏差纠正下的地统计反演模拟BGIM（Bias-corrected Geostatistical Inverse Model）降尺度算法研究。试验同时引入AERONET地基观测数据和MODIS 3 km DT AOD数据产品作为降尺度结果的绝对与相对验证标准。结果表明：季节偏差系数纠正下生成的MODIS 3 km DT_DB_Combined AOD与10 km DT_DB_Combined AOD、3 km DT AOD数据产品的绝对精度相当,验证R²分别为0.79、0.70、0.71;且相比MODIS 3 km DT AOD数据产品,季节偏差系数纠正下的MODIS 3 km DT_DB_Combined AOD数据与其相关系数可达0.93;在时间覆盖度和空间覆盖度方面可分别提升11.21%和11.44%,其中春、冬两季空间覆盖度提升效果尤为显著。研究结果证实BGIM降尺度算法可有效估算MODIS 3 km DT_DB_Combined AOD数据,提高MODIS 3 km AOD产品的时空覆盖度,并同时抑制原有MODIS 10 km DT_DB_Combined AOD数据产品的季节性高估现象。  相似文献   

单基线TanDEM-X InSAR相干性反演森林高度EI北大核心CSCD     

张涛  朱建军  付海强  汪长城 《测绘学报》2022,51(9):1931-1941

由RVoG模型演变的SINC函数模型运用到TanDEM-X InSAR数据反演森林高度时面临观测信息不足的问题,且无法适应不同的森林场景。本文针对这一问题,提出小范围LiDAR数据辅助下基于TanDEM-X InSAR相干性的森林高度反演方法,此方法无须全局高精度DEM产品提供地表相位信息而仅利用相干性即可获取森林高度信息。为验证此方法的可行性,采用西班牙境内两个典型试验区的TanDEM-X InSAR数据进行验证,并利用LiDAR树高数据进行精度评定。结果表明,单基线TanDEM-X InSAR相干性可用于反演森林高度,两个试验区的精度分别为2.34 m和1.74 m。  相似文献   

新疆西准噶尔达尔布特蛇绿岩套柳树沟镁铁质杂岩SHRIMP锆石U-Pb年龄及地球化学特征     

李纲  ;杨斌  ;梁恩云  ;马铁球  ;曹顺红 《华南地质与矿产》2014,(3):194-205

对新疆西准噶尔达尔布特蛇绿岩套柳树沟镁铁质杂岩中橄榄辉长岩、蛇纹石化橄榄辉长岩、辉长岩和蚀变辉长岩地球化学分析表明:辉长岩和蚀变辉长岩具有钙碱性和拉斑玄武岩的双重特征,橄榄辉长岩和蛇纹石化橄榄辉长岩属镁铁质堆积岩,为蛇绿岩组成单元;稀土总量较高,具微弱正Eu异常,稀土元素配分模式为略左倾平坦型,与SSZ型镁铁质堆晶岩稀土配分模式相同;微量元素蛛网图上,富集大离子亲石元素Cs、K、Th、U,相对亏损高场强元素Nb、Ta,可能代表俯冲板片的流体交代上覆地幔楔使地幔岩石发生部分熔融。地球化学构造环境判别柳树沟镁铁质岩石岩浆源区为亏损型地幔向富集型地幔过渡的适度富集型地幔,其形成的最佳模型是在成熟岛弧基础上裂谷化形成的一个不成熟的类似边缘海性质弧后盆地,不具成熟大洋或盆地那样的洋壳-上地幔结构,在盆地扩张初期岩浆具岛弧特征,随着盆地被进一步打开,镁铁质岩石具N-MORB特征。对辉长岩采用SHRIMP锆石U-Pb同位素年龄测试,获得特柳树沟镁铁质岩石的结晶时间为314.9±1.7 Ma。  相似文献   

Going green or going away: Environmental regulation,economic geography and firms’ strategies in China’s pollution-intensive industries     

《Geoforum》2014

The high-growth, resource- and pollution-intensive industrialization model that China has pursued has caused severe environmental pollution and deterioration, particularly in a number of clusters in the coastal regions of East and Southeast China, where the Reform and Opening-up policies first started. The lack of uptake of environmental norms/values, deficit of regulatory enforcement of environmental policies, and insufficient institutional capacity have been compounding factors. As environmental standards were raised by China’s central government, the enforcement of environmental regulation has been compromised more in inland China than in coastal regions, due to China’s “decentralized governance structure” and regional disparity in terms of both economic development and environmental pollution. This paper therefore argues that rising environmental regulations, as well as firm characteristics, regional hub effect and political environment, have all been particularly important in forcing China’s pollution-intensive enterprises to restructure their production, through innovation, upgrading, geographical relocation, outsourcing and plant closure, especially in China’s coastal regions. It contributes to recent studies by developing a heuristic analytical framework that aims to be sensitive to the impacts of environmental regulation, political environment and regional hub effect over firm restructuring, but which does so by stressing these impacts are simultaneously inflected by the nature and attributes of firms. The empirical analysis suggests a roughly inverted “U”-shaped relationship between firm relocation tendency and firm size (or firm capability), resulting from complex interactions between political environment, regional hub effect and environmental regulation.  相似文献   

Geology and genesis of the Hehuaping magnesian skarn-type cassiterite-sulfide deposit,Hunan Province,Southern China     

《Ore Geology Reviews》2014

Magnesian skarn-type tin deposits are relatively rare in the world. The Hehuaping cassiterite-sulfide deposit in southern China, having a total reserve of approximately 130,000 t of tin, 50,000 t of lead and 10,000 t of zinc, is identified as such type. The deposit is related to the Late Jurassic (157 Ma) Hehuaping medium- to coarse-grained biotite granite that intruded the Middle Devonian Qiziqiao dolomite Formation and the Tiaomajian sandstone Formation. Four paragenetic stages of skarn and ore formation have been recognized: I. prograde stage, II. retrograde stage, III. cassiterite-sulfide stage and IV. carbonate stage. Alteration zoning between fresh granite and unaltered country rocks can be identified. The skarn are typified by Mg-mineral assemblages of forsterite, spinel, diopside, tremolite, serpentine, talc, and phlogopite. The geochemistry of various skarn minerals shows a gradually decrease of Mg end member and, correspondingly, an increase of Fe- and especially Mn end members along the process of skarn alteration.Tin mineralization developed during the late retrograde stage resulted in cassiterite–magnetite-diopside skarn. However, the deposition of cassiterite occurred predominantly as cassiterite-sulfide veins along fractures and interlayer fracture zones during stage III. The petrogeochemistry of Hehuaping granite, as well as S- and Pb isotopic analyses suggest that the ore-forming elements have a magmatic source originated from the upper crust. The HO isotopic and fluid-inclusion analyses indicate that high-temperature ore-forming fluids in early anhydrous skarn stage (stage I) are also magmatic origin. In comparison, the retrograde fluids are characterized by relatively low salinity (2 to 10 wt.% NaCl equiv) and low temperature (220 to 300 °C), suggesting a mixed origin of meteoric waters with magmatic fluids. The major ore-forming stage III fluids are characterized by lower temperature (170 to 240 °C) and salinity (1 to 6 wt.% NaCl equiv), indicating fluid mixing could be an efficient tin-mineralizing mechanism. Meteoric waters are dominant in stage IV, resulting in a further lowering of temperature (130 to 200 °C) and salinity (0.4 to 1 wt.% NaCl equiv).  相似文献   

湘西大溶溪钨矿床中辉钼矿Re-Os同位素定年及其地质意义   总被引：9，自引：2，他引：7  

张龙升  彭建堂  胡阿香  林芳梅  张婷 《矿床地质》2014,33(1):181-189

湘西大溶溪钨矿床,为雪峰隆起区内的一个中型白钨矿矿床。文章对该矿床中穿插钨矿体的含辉钼矿石英脉进行了Re-Os同位素年代学研究。分析结果显示,该矿中辉钼矿的Re-Os同位素模式年龄为217.0~221.1 Ma,平均为（219.0±1.2） Ma,其对应的等时线年龄为（223.3±3.9） Ma,揭示其形成于晚三叠世。这些年龄数据与矿区内大神山花岗岩的侵位时间〔（224.3±1.0） Ma〕基本吻合,表明该区含辉钼矿石英脉的形成与花岗岩的侵位具有密切的时、空联系。考虑到该区钨矿体的形成时间介于花岗岩和含辉钼矿石英脉之间,因此,推断大溶溪钨矿床形成于223 Ma左右。该研究成果,不仅为湘西雪峰隆起区存在多期次的钨成矿事件提供了可靠证据,同时又进一步证实了华南地区确实存在一次区域性的与印支期花岗岩有关的成矿作用。  相似文献   

Dynamic Brazilian Tests of Granite Under Coupled Static and Dynamic Loads   总被引：2，自引：2，他引：0  

Zilong Zhou  Xibing Li  Yang Zou  Yihui Jiang  Guonan Li 《Rock Mechanics and Rock Engineering》2014,47(2):495-505

Rocks in underground projects at great depth, which are under high static stresses, may be subjected to dynamic disturbance at the same time. In our previous work (Li et al. Int J Rock Mech Min Sci 45(5):739–748, 2008), the dynamic compressive behaviour of pre-stressed rocks was investigated using coupled-load equipment. The current work is devoted to the investigation of the dynamic tensile behaviour of granite rocks under coupled loads using the Brazilian disc (BD) method with the aid of a high-speed camera. Through wave analyses, stress measurements and crack photography, the fundamental problems of BD tests, such as stress equilibrium and crack initiation, were investigated by the consideration of different loading stresses with abruptly or slowly rising stress waves. The specially shaped striker method was used for the coupled-load test; this generates a slowly rising stress wave, which allows gradual stress accumulation in the specimen, whilst maintaining the load at both ends of the specimen in an equilibrium state. The test results showed that the tensile strength of the granite under coupled loads decreases with increases in the static pre-stresses, which might lead to modifications of the blasting design or support design in deep underground projects. Furthermore, the failure patterns of specimens under coupled loads have been investigated.  相似文献   

Dynamic Indirect Tensile Strength of Sandstone Under Different Loading Rates   总被引：1，自引：1，他引：0  

Feng-Qiang Gong  Gao-Feng Zhao 《Rock Mechanics and Rock Engineering》2014,47(6):2271-2278

  相似文献   

招平断裂带中段断裂成矿有利度分析          下载免费PDF全文

吴泽权  毛先成  陈进  陈东锋  成功 《地质找矿论丛》2014,29(1):44-50

招平断裂带是我国著名的金矿成矿带。断裂的空间展布形态特征对寻找断裂构造控矿型金矿床具有重要作用。通过断裂的遥感解译,研究了招平断裂带主断裂的走向、主断裂地表破碎带宽度以及主断裂起伏程度等成矿有利度指标,构建了基于断裂距离场的成矿有利度分析模型,并圈定研究区域成矿远景区11处,为区域地质、物化探等勘查工作提供了指导性意见。  相似文献   

椭球体的视电阻率特征     

张超  汤井田  强建科 《物探化探计算技术》2014,(2):158-163

椭球体是最具代表性的典型三维地电体之一,它三个轴的长短经过变化后可以和多种形状的地电体相似。因此,实现了椭球体电阻率的求解,就可以模拟绝大多数三维地电体的电阻率曲线。从拉普拉斯方程的求解出发,得到了均匀空间中存在的水平椭球体异常表达式,并用简单加倍的方法得到了均匀半空间中水平椭球体的视电阻率公式,结合倾斜旋转椭球体的视电阻率公式的规律,得到了倾斜椭球体的视电阻率公式,再进行一系列简化得到板状体。最后分析对比了均匀电场中旋转椭球体和板状体的视电阻率曲线的形态和规律。结论表明:旋转椭球体与板状体的视电阻率曲线的走向大体相似,且板状体的曲线相比旋转椭球体较缓和。对于低阻情况,在异常体顶部附近的视电阻率异常为零,异常体的倾向一侧有极小值,反倾向一侧有极大值,曲线随倾角α的增大而逐渐变陡。对于高阻情况,视电阻率的极大值出现在异常体顶部附近,两侧有极小值,倾向一侧的曲线较缓和而反倾向一侧的曲线较陡峭,随着倾角α的增大,视电阻率异常变大。  相似文献