青藏高原中部日干配错断裂第四纪活动特征及2020年7月23日西藏尼玛Mw6.4地震发震构造分析     

刘富财  潘家伟  李海兵  孙知明  刘栋梁  卢海建  郑勇  王世广  白明坤  Marie-Luce CHEVALIER  张蕾  曹勇 《地球学报》2022,43(2):173-188

日干配错断裂位于青藏高原中部, 是"V"型共轭走滑构造中班公湖—怒江缝合带以北的一条NEE-SWW走向左行走滑断裂, 在调节青藏高原南北向挤压和东西向伸展过程中起着重要的作用.在2008年1月9日及2020年7月23日, 先后在该断裂南西端和北东支分别发生6级以上强震.因此, 查明该断裂的晚第四纪活动性及其与区域强震活...  相似文献   

Holocene slip rate of northern Gyaring Co Fault along Karakorum-Jiali Fault Zone (KJFZ), in central Tibet     

WANG Duo  YIN Gongming  JIANG Yafeng  HAN Fei  CHUNG Lingho 《《地质学报》英文版》2013,87(Z1):391-392

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面向城市地物分类的 SAR 图像纹理特征提取与分析     

程雪姣  徐佳  刘庆群  陆吉 《东北测绘》2014,(4):47-50

合成孔径雷达（ SAR）图像含有丰富的纹理信息,特别是进行城市地物分类时,纹理特征对于图像的解译具有重要的意义。本文对基于灰度共生矩阵和Gabor变换两种纹理特征提取方法进行了研究,将灰度和不同纹理特征组合应用于SAR图像城市地物分类,并以ALOS PALSAR影像为数据源进行了实验。通过对不同分类结果进行定性和定量分析,结果表明,引入纹理特征后的SAR图像分类结果要优于无纹理信息参与的分类结果,基于不同纹理特征组合的SAR图像分类结果要优于基于单一纹理特征的分类结果。  相似文献   

藏南普莫雍错流域水体离子组成与空间分布及其环境意义(英文)   总被引：2，自引：1，他引：1  

朱立平  鞠建廷  汪勇  谢曼平  王君波  彭萍  甄晓林  林晓 《地理学报(英文版)》2010,20(1):109-120

The chemistry of major cations (Mg²⁺, Ca²⁺, Na⁺, and K⁺) and anions (HCO₃ ⁻, SO₄ ²⁻, and Cl⁻) in the water of Lake Pumayum Co and its inflow river was studied, revealing the obvious ionic difference among various inflow rivers and the lake. The chemical type of the lake water was Mg²⁺-Ca²⁺-HCO₃ ⁻-SO₄ ²⁺, but the major ions of the main inflow rivers were Ca²⁺-Mg²⁺-HCO₃ ⁻. In the lake inlet of Jiaqu River, the main inflow river, there was significant variance of water chemistry within the depth less than 2 m. However, it was almost homogeneous at other area of the lake. Therefore, with the evidence of distribution of water chemistry and oxygen isotope of lake water, a conclusion can be outlined that Jiaqu River had a distinct effect on the hydrochemistry of the water on the submerged delta, whereas this is not the case for other rivers. The Gibbs plot revealed that the dominant mechanism responsible for controlling chemical compositions of the lake water was rocks weathering in the drainage area. Ion ratios and ternary plots further explored the main processes controlling the water chemistry of the catchment, i.e., carbonate weathering, pyrite weathering, and silicate weathering. The different hydrochemistry characteristics between river water and lake water may result from the CaCO₃ precipitation. The findings will benefit the explanation of the environmental significance of carbonate in paleolimnological studies in the lake.  相似文献   

Co‐Composting of Macrophyte Biomass and Sludge as an Alternative for Sustainable Management of Constructed Wetland By‐Products          下载免费PDF全文

Soulwène Kouki  Neila Saidi  Fadhel M'hiri  Amor Hafiane  Abdennaceur Hassen 《洁净——土壤、空气、水》2016,44(6):694-702

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L-半胱氨酸缩邻香草醛Co(Ⅱ)配合物的合成、表征及与DNA的作用研究     

董丽丽  范玉华  刘善斌  张霞  毕彩丰 《中国海洋大学学报(自然科学版)》2012,42(6):107-112

制备了L-半胱氨酸缩邻香草醛配体C11H13NO4S,将其与Co(Ⅱ)作用合成了一种新型的配合物.通过元素分析、核磁共振、红外光谱、紫外-可见光谱、摩尔电导率分析及TG-DTG等手段对合成的配合物进行了表征.双核配合物的组成为[Co2(C11H12NO4S)2 (CH3COO)2],配体中的酚羟基的氧原子,氨基上的氮原子分别参与配位,羧基以双齿形式参与配位,Co(Ⅱ)的配位数为6.利用紫外-可见光谱,荧光发射光谱,离子强度改变,[Fe(CN)6]4荧光猝灭及黏度测定等方法对Co(Ⅱ)配合物与小牛胸腺DNA(CT-DNA)的结合方式进行了研究.实验结果表明,Co(Ⅱ)配合物与CT-DNA的结合方式为插入结合.  相似文献   

The response of lake-glacier variations to climate change in Nam Co Catchment,central Tibetan Plateau,during 1970–2000   总被引：1，自引：0，他引：1  

Yanhong Wu  Liping Zhu 《地理学报(英文版)》2008,18(2):177-189

Based upon the 1970 aero-photo topographic map, and TM/ETM satellite images taken in 1991 and 2000, the authors artificially interpreted boundaries of lake and glaciers in Nam Co Catchment, and quantified lake-glacier area variations in different stages by ＂integrated method＂ with the support of GIS. Results show that from 1970 to 2000, lake area increased from 1942.34 km^2 to 1979.79 km^2 at a rate of 1.27 km^2/a, while glacier area decreased from 167.62 km^2 to 141.88 km^2 at a rate of 0.86 km^2/a. The increasing rate of lake in 1991-2000 was 1.76 km^2/a that was faster than 1.03 km^2/a in 1970-1991, while in the same period of time, the shrinking rates of glaciers were 0.97 km^2/a and 0.80 km^2/a respectively. Important factors, relevant to lake and glacier response to the climate, such as air temperature, precipitation, potential evapotranspiration and their values in warm and cold seasons, were discussed. The result suggests that temperature increasing is the main reason for the accelerated melting of glaciers. Lake expansion is mainly induced by the increase of the glacier melting water, increase of precipitation and obvious decrease of potential evapotranspiration. Precipitation, evaporation and their linkages with lake enlargement on regional scale need to be thoroughly studied under the background of global warming and glacier retreating.  相似文献   

近46年松木希错流域冰川和湖泊变化及原因分析     

李治国  芦杰  史本林  李红忠  张延伟  李琳 《地理研究》2015,34(11):2095-2104

采用1:5万地形图、Landsat MSS/TM/ETM+/OLI遥感影像及数字高程模型数据,利用遥感和地理信息系统技术,并结合狮泉河、和田和于田3个气象站点1968-2013年的气温、降水量数据对松木希错流域的冰川、湖泊面积变化及其原因进行分析。结果表明：① 1968-2013年流域冰川面积不断退缩,由139.25 km²减少至137.27±0.02 km²,共减少1.98±0.02 km²,减少百分比为1.42%,2001年以后冰川退缩速度加快;② 1968-2013年松木希错面积不断扩张,由25.05 km²增加至32.62±0.02 km²,共扩张7.57±0.02 km²,扩张百分比为30.22%,且2001年之后扩张速率加快,在年代际上与冰川的退缩具有较好的耦合性;③ 1968-2013年湖面潜在蒸散量减少和降水增加分别是导致湖泊扩张的第一和第二影响因素,而升温引起的冰川、冻土融水增加有一定贡献,但影响较小且在年际尺度上不显著。  相似文献   

酒泉钢铁公司地下水源地数值模拟及水位预报   总被引：1，自引：1，他引：0       下载免费PDF全文

张举  丁宏伟  蒲晓斌  陈治国 《甘肃地质》2005,14(2):76-81

依据实际勘察资料,在全面阐述供水水源地水文地质条件及开采状况,进行地下水均衡计算的基础上,建立了勘察区地下水二维流水量数学模拟模型,重点以酒钢近期和远期对地下水资源的需求量2个开采方案为依据,利用模型对未来水源地地下水位的变化趋势和特征进行了预测预报。结果表明,各水源地总计按近期27.648万m3/d开采至2030年,开采区最大水位降深小于设计允许降深12m,并均已形成稳定的降落漏斗,由此引起的泉水溢出量减少对酒泉西盆地生态环境基本无影响,对现有的其它水源地影响甚微。而各水源地总计按远期34.56万m3/d开采至2030年,北大河、嘉峪关水源地开采井降深小于设计允许降深,自2011年降落漏斗已基本稳定,但黑山湖水源地开采降落漏斗中心最大水位降深分别为17.22m和23.60m,远大于设计允许降深,并且地下水位持续下降,降落漏斗不断扩大并与北大河、嘉峪关水源地降落漏斗相连形成区域性大降落漏斗,由此引起的水位降幅将使现有的泉水大量衰减直至完全消失,对下游生态环境将产生巨大的负面影响。为实现水资源的永续利用和酒钢经济的可持续发展,酒泉公司未来必须实施开源与节流并具的用水战略。  相似文献   

Experimental Investigation and Kinetic Modeling of p‐Nitrophenol and Phenol by Kissiris‐Immobilized Ralstonia eutropha in a Batch Reactor          下载免费PDF全文

Mahdi Motamedi  Alireza Habibi  Mohammad Maleki  Farzaneh Vahabzadeh 《洁净——土壤、空气、水》2015,43(2):237-243

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