东亚地区春季黑碳气溶胶源排放及其浓度分布   总被引：25，自引：1，他引：24       下载免费PDF全文

张美根  徐永福  张仁健  韩志伟 《地球物理学报》2005,48(1):46-51

本研究收集整理了东亚地区一个黑碳气溶胶的排放源,并利用一个三维化学输送模式系统模拟研究了东亚地区春季黑碳气溶胶的输送和演变过程.黑碳气溶胶浓度的模拟值与地面观测站和观测船获取的监测值相比,模拟值与监测值具有良好的一致性,这表明本研究收集整理的黑碳气溶胶的排放量及其分布是基本合理的,模式系统较好地反映了黑碳气溶浓度的时空分布和变化趋势,再现了许多观测到的重要特征.模拟结果表明,东亚地区春季间隙性的长距离输送对于西北太平洋海域的黑碳气溶胶浓度分布具有非常重要的影响.  相似文献   

基于吉布斯抽样的相关观测异常值检测的贝叶斯方法     

魏萌  王靳辉  衡广辉 《测绘科学技术学报》2012,(5):326-329

相关观测的异常值检测是测量数据处理的难题之一。在系统总结和分析前人研究成果的基础上,运用贝叶斯统计推断理论,提出了相关观测异常值检测的贝叶斯方法。首先,基于识别变量的后验概率,提出了相关观测异常值定位的贝叶斯方法;然后设计和构建了计算后验概率的吉布斯抽样方法,基于最大后验估计原理,推导和建立了计算异常值参数的贝叶斯公式;最后对某GPS网相连进行了计算和分析。结果表明,在相关观测条件下,使用新方法能够对多个异常值同时进行检测,有效地消除异常值的不良影响。  相似文献   

Evaluation of WRF Model Hydrometeors Based on TMI Observations Using an Indirect Method          下载免费PDF全文

FU Yun-Fei  HENG Zhi-Wei  LI Tian-Yi  SHEN Zhong-Ping  WANG Yu 《大气和海洋科学快报》2012,5(1):32-37

Using a microwave radiative transfer(MWRT) model with microwave brightness temperatures(TBs) observed from the Tropical Rainfall Measuring Mission(TRMM) Microwave Imager(TMI),an indirect approach evaluated hydrometeors generated from the Weather Research and Forecasting(WRF) model in the process of CHABA typhoon in August 2004.This study compares the simulated TBs generated from the microwave radioactive transfer model connected to the WRF model with the observed TBs derived from TMI and analyzes the differences between these TBs.The results indicate that the WRF model underestimates the amount and area of liquid and ice hydrometeors inside the typhoon center.The results also indicate relatively better agreement between the simulated and the observed TBs in the vertical polarization than in the horizontal polarization.  相似文献   

致密砂岩气藏地层水水化学特征及其地质意义——以川西坳陷新场气田为例     

山俊杰  黄仕林  毕有益  邓美洲  严焕榕  衡勇  郑艳 《岩石矿物学杂志》2024,43(1):63-73

四川盆地侏罗系沙溪庙组及三叠系须家河组作为陆上致密气资源增储上产重点的接替区,保有大量的难动用储量,具有较大的勘探开发潜力。然而随着深入的滚动勘探开发,中浅层沙溪庙组气藏和深层须家河组气藏气井产水已严重制约了气井产能,部分气井甚至因水淹而停产。本文对研究区不同层位34口气井的地层水进行了主量、微量元素和气藏成藏演化特征分析,结果显示沙溪庙组气藏和须家河组气藏经历了先成藏后致密再改造的成藏演化过程,断层的沟通导致深层须家河组地层水的大量上涌,使断层附近高渗的砂体被充注,在水动力等驱动作用下,天然气以游离相或水溶相沿断裂带进行垂向高效运移。垂向上大部分离子含量都随着埋深逐渐增大,深层须家河组地层水气藏具有较好的油气保存条件,并且经历了更为复杂的水岩相互作用,不同程度地使K、Ba、Sr、Li、Rb等元素更加富集。  相似文献   

Geochemistry and Petrogenesis of the Tongshankou and Yinzu Adakitic Intrusive Rocks and the Associated Porphyry Copper-Molybdenum Mineralization in Southeast Hubei, East China   总被引：11，自引：0，他引：11  

Qiang Wang    Zhen-Hua Zhao    Zhi-Wei Bao    Ji-Feng Xu    Wei Liu  Chao-Feng Li  Zheng-Hua Bai  Xiao-Lin Xiong 《Resource Geology》2004,54(2):137-152

Abstract. The late Jurassic Tongshankou and Yinzu plutons in southeast Hubei have been investigated for their contrasting metal mineralization features. The former is closely associated with porphyry Cu‐Mo mineralization, while the latter is barren of metal mineralization, althouth both are located very close to each other. The Tongshankou granodiorite porphyries and the Yinzu granodiorites are geochemically similar to adakites, e.g., high Al₂O₃ and Sr contents and La/Yb and Sr/Y ratios, enriched in Na₂O, depleted in Y and Yb, very weak Eu anomalies and positive Sr anomalies. However, different geochemi‐cal characteristics exist between the two plutons: the Tongshankou adakitic rocks (1) are relatively enriched in SiO₂, K₂O, MgO, Cr, Ni, and Sr and depleted in Y and Yb; (2) have higher degree REE differentiation; (3) have positive Eu anomalies in contrast with very weak negative or unclear Eu anomalies in the Yinzu rocks; and (4) isotopically have relatively higher eP_Nd(t) values (‐5.19 to ‐5.38) and lower initial ⁸⁷Sr/⁸⁶Sr ratios (0.7060 to 0.7062), while the Yinzu adakitic rocks have relatively lower eP_Nd(t) values (‐7.22 to ‐8.67) and higher initial ⁸⁷Sr/⁸⁶Sr ratios (0.7065 to 0.7074). The trace element and isotopic data demonstrate that the Tongshankou adakitic rocks were most probably originated from partial melting of delaminated lower crust with garnet being the main residual mineral whereas little or no plagioclase in the source. On the contrary, the Yinzu adakitic rocks were likely derived from partial melting of thickened lower crust, with residual garnet and a small quantity of plagioclase and hornblende in the source. Interactions between the adakitic magmas and mantle peridotites possibly took place during the ascent of the Tongshankou adakitic magmas through the mantle, considering that MgO, Cr, and Ni contents and eP_Nd(t) values of the adakitic magmas were possibly elevated and initial ⁸⁷Sr/⁸⁶Sr ratios were possibly lowered due to the contamination of mantle peridotites. In addition, the Fe₂O₃ of the adakitic magmas was likely released into the mantle and the oxygen fugacities (?_o2) of the latter were obviously possibly raised, which made metallic sulfide in the mantle oxidized and the chalcophile elements such as Cu were incorporated into the adakitic magmas. The ascent of the adakitic magmas enriched in Cu and Mo will lead to the formation of porphyry Cu‐Mo deposit. Nevertheless, the Yinzu adakitic magmas were possibly lack of metallogenetic materials due to not interacting with mantle peridotite, and thus unfavorable to metal mineralization.  相似文献   

Alkaline syenites in eastern Cathaysia (South China): link to Permian–Triassic transtension     

Qiang Wang  Jian-Wei Li  Ping Jian  Zhen-Hua Zhao  Xiao-Lin Xiong  Zhi-Wei Bao  Ji-Feng Xu  Chao-Feng Li  Jin-Long Ma 《Earth and Planetary Science Letters》2005,230(3-4):339-354

Two alkaline syenite plutons, the Tieshan and Yangfang plutons, have recently been recognized within NE-trending fault zones in eastern Cathaysia, South China. The rocks are very enriched in K₂O (6.28–9.39 wt.%), rare earth elements (REE; particularly light REE) and large ion lithophile elements, but are relatively low in high field strength elements. Isotopically, they are characterized by high initial ⁸⁷Sr/⁸⁶Sr (0.7093 to 0.7123) and low _Nd(t) values (−5.64 to −10.63). The geochemical data suggest that the alkaline syenites most likely formed via fractional crystallization of enriched mantle-derived magmas. Sensitive High-Resolution Ion Microprobe zircon U–Pb dating indicates that these two intrusions have Late Permian (254±4 Ma) and Early Triassic (242±4 Ma) crystallization ages, respectively. Our data suggest that a tectonic regime dominated by transtension probably existed from at least the latest Permian into the Triassic and was responsible for the formation of the Tieshan and Yangfang alkaline syenites. When combined with previous paleomagnetic, structural, and sedimentology data, we suggest that the transtension along the NE-trending strike-slip fault zones was related to oblique subduction of the Pacific plate underneath South China.  相似文献   

中国的空间环境研究   总被引：1，自引：0，他引：1       下载免费PDF全文

叶宗海  都亨 《地球物理学报》1997,40(Z1):429-441

主要介绍我国的空间环境研究及其进展，包括空间环境探测，特别是利用卫星探测；空间环境资料和模式的收集与研究；空间环境与航天器的相互作用及其对航天器的影响；以及空间环境预报等．  相似文献   

盐水泥浆测井解释技术分析     

衡志 《地球物理学报》1990,33(1):77-86

大港油田盐水泥浆测井解释评价工作已有20余年的历史.本文论述在盐水泥浆中“时间推移测井”解释技术及“粗、细粒、低矿化度地层水的砂岩储集层复杂油层评价的新技术”.这些技术已在该油田使用,并经试油资料验证,油层解释符合率由原来的56.5％上升为93.6％,获得了显著的地质效果.  相似文献   

近50年东北冷涡异常特征及其与前汛期华南降水的关系分析   总被引：16，自引：11，他引：16  

苗春生  吴志伟  何金海  池艳珍 《大气科学》2006,30(6):1249-1256

利用中国气象局国家气象信息中心提供的1951～2004年中国160站华南前汛期 (5～6月) 月平均降水、气温资料、欧洲中心提供的ERA-40再分析资料和Reynolds海温资料, 对东北冷涡与华南前汛期降水进行了统计分析, 定义了一个前汛期东北冷涡强度指数 (NECVI), 并研究了前汛期东北冷涡异常年同期东亚季风、西太平洋副高、对流层低层的垂直运动异常特征和前期全球海表温度 (SST) 的先兆信号, 结果表明: 前汛期东北冷涡强度与华南降水存在显著的正相关, 东北冷涡强年, 前期东亚冬季风偏弱, 同期东亚夏季风异常爆发提前且偏强, 西太平洋副高位置偏南, 华南地区低层上升运动发展, 降水偏多; 东北冷涡偏弱年, 前期东亚冬季风偏弱, 同期东亚夏季风爆发推迟且偏弱, 西太平洋副高位置偏北, 华南地区低层下沉运动发展, 降水偏少; 前汛期东北冷涡与前期中国近海海温存在显著的负相关关系, 前汛期东北冷涡异常强年, 前期对应着La Nia的成熟阶段或发展阶段, 而前汛期东北冷涡异常弱年则对应着El Nio的成熟阶段或发展阶段.  相似文献   

基于远震接收函数的南极大陆冰盖厚度研究   总被引：1，自引：1，他引：0       下载免费PDF全文

晏鹏  李志伟  李斐  杨元德  郝卫峰  周磊 《地球物理学报》2017,60(10):3780-3792

冰盖厚度是研究南极冰盖质量、建立冰盖动力学模型的基本参数,对于冰川均衡调整、冰盖物质平衡及全球气候变化研究具有重要意义.基于地震学的远震接收函数和H-Kappa格网搜索方法可以用于地震台站下方冰盖厚度的可靠探测,不仅能与冰雷达获得的冰盖厚度进行独立对比,还可以与冰雷达方法相互补充,进一步填补南极大陆冰盖厚度探测空白区.本文利用布设于南极大陆冰盖上方的流动地震台阵记录到的远震波形数据,基于接收函数方法对台阵下方的冰盖厚度进行了研究.结果显示:基于远震接收函数方法的冰盖厚度与Bedmap2冰厚格网模型相比,二者差别大多在200 m以内;少数台站差值达到600 m左右,这一差别可能与Bedmap2测线分布空区、冰雷达测深不确定性以及冰盖内部复杂波速结构等因素有关.本文研究结果表明:利用南极大陆冰盖上方的流动地震台阵,基于远震接收函数方法可以获得比较可靠的南极冰盖厚度,为独立验证冰雷达的探测结果并弥补冰雷达探测空白区提供了有效方法.同时,部分台站接收函数波形的复杂性可能暗示了南极大陆数千米厚的冰盖内部结构不是均一的,仍然存在比较复杂的内部结构变化.因此,有必要进一步利用包括接收函数波形拟合、地震面波反演等方法对南极大陆冰盖厚度及其内部精细结构进行更为深入的研究.  相似文献