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961.
三峡水库自2003年蓄水以来,水库干支流水环境状况及水华已成为广泛关注的问题,国内外不少学者对此开展了大量研究。本文回顾了近20年来三峡水库水环境相关研究,系统总结了三峡水库干支流水动力特征及其生态环境影响,并展望了三峡水库水动力相关研究的新视角、新内容、新方法、新技术。结果表明:(1)三峡水库蓄水后干支流水流分化特征明显,干流水体从上游的河流型水体逐渐转变为坝前的过渡型水体,而支流库湾则更偏向于湖泊型水体特征;(2)干支流密度差(温度差)驱动的分层异重流,水库日调节调度驱动的高频水流振荡,气象驱动的近表层水体混合是三峡水库支流库湾普遍存在的水动力现象,主导着支流库湾的水温分层和混合过程;(3)三峡水库特殊的水动力现象对支流库湾水温分层结构、营养盐输移补给、水华生消过程、温室气体排放等产生深远影响,应用生态调度调控支流库湾水动力过程来改善其水环境问题已成为该区域生态环境修复的重要技术手段。如何将上述新发现上升为具有三峡水库特色的系统理论与方法,并形成大型深水水库生态环境研究技术体系,服务于大型梯级水库群联合多目标优化调度实践,仍是今后努力的方向。 相似文献
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964.
The Seismic Induced Soft Sediment Deformation Structures in the Middle Jurassic of Western Qaidamu Basin 总被引:1,自引:0,他引:1
Intervals of soft-sediment deformation structures are well-exposed in Jurassic lacustrine deposits in the western Qaidamu basin. Through field observation, many soft-sediment deformation structures can be identified, such as convoluted bedding, liquefied sand veins, load and flame structures, slump structures and sliding-overlapping structures. Based on their genesis, soft-sediment deformation structures can be classified as three types: seismic induced structures, vertical loading structures, and horizontal shear structures. Based on their geometry and genesis analysis, they are seismic-induced structures. According to the characteristics of convoluted bedding structures and liquefied sand veins, it can be inferred that there were earthquakes greater than magnitude 6 in the study area during the middle Jurassic. Furthermore, the study of the slump structures and sliding-overlapping structures indicates that there was a southeastern slope during the middle Jurassic. Since the distance from the study area to the Altyn Mountain and the Altyn fault is no more than 10km, it can be also inferred that the Altyn Mountain existed then and that the Altyn strike-slip fault was active during the middle Jurassic. 相似文献
965.
A method to estimate concentrations of surface-level particulate matter using satellite-based aerosol optical thickness 总被引:3,自引:0,他引:3
TAO JinHua ZHANG MeiGen CHEN LiangFu WANG ZiFeng SU Lin GE Cui HAN Xiao ZOU MingMin 《中国科学:地球科学(英文版)》2013,(8):1422-1433
We propose a new method to estimate surface-level particulate matter(PM)concentrations by using satellite-retrieved Aerosol Optical Thickness(AOT).This method considers the distribution and variation of Planetary Boundary Layer(PBL)height and relative humidity(RH)at the regional scale.The method estimates surface-level particulate matter concentrations using the data simulated by an atmospheric boundary layer model RAMS and satellite-retrieved AOT.By incorporation MODIS AOT,PBL height and RH simulated by RAMS,this method is applied to estimate the surface-level PM 2.5 concentrations in North China region.The result is evaluated by using 16 ground-based observations deployed in the research region,and the result shows a good agreement between estimated PM 2.5 concentrations and observations,and the coefficient of determination R2 is 0.61 between the estimated PM 2.5 concentrations and the observations.In addition,surface-level PM 2.5 concentrations are also estimated by using MODIS AOT,ground-based LIDAR observations and RH measurements.A comparison between the two estimated PM 2.5 concentrations shows that the new method proposed in this paper is better than the traditional method.The coefficient of determination R2 is improved from 0.32 to 0.62. 相似文献
966.
967.
Cooling and exhumation of the oldest Sanqiliu uranium ore system in Motianling district,South China Block 总被引:2,自引:0,他引:2
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Liang Qiu Dan‐Ping Yan Shuang‐Li Tang Nicholas T. Arndt Li‐Ting Fan Qing‐Yin Guo Jian‐Yong Cui 《地学学报》2015,27(6):449-457
The Sanqiliu uranium deposit belongs to a uranium ore system in Motianling district. It is the oldest uranium deposit in South China. Primary uranium mineralization occurred almost simultaneously with the emplacement of the host granites and subsequent dykes, and it has a relatively high grade of uranium (0.421%). We clarify the age of mineralization and investigate the cooling history through new pitchblende U–Pb and apatite fission‐track thermochronology. The pitchblende U–Pb results indicate that uranium mineralization occurred at ~801–759 Ma. Fractionation of uranium and lead at ~374–295 Ma is interpreted as remobilization and resetting of the original uranium. The Motianling area has apatite fission‐track ages of 57 to 18 Ma. By combining our results with previous work, we conclude that the deposit cooled slowly and was exposed at the surface during the Cenozoic. The timing and depth of exhumation helped to preserve and avoid erosion of the uranium deposit, and highlight the potential for regional uranium exploration. 相似文献
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969.
利用天津地震台网2002-2007年记录到的天津及周边地区,ML≥1.5地震。在天津及周边地区,按照活动空间分布特征圈定4个区域,采用单事件多台观测资料,对所选区域里的地震事件进行平均波速比值的计算,得到天津地区波速比变化与地震的对应关系。 相似文献
970.
CD-L1型流气式固体氡源替换RN-150型氡源的研究 总被引:1,自引:0,他引:1
通过对CD-L1型流气式固体氡源氡产生率稳定性、同一闪烁室用不同氡源标定K值的对比实验研究,表明用CD-L1型流气式固体氡源与用RN-150型氡源标定的K值之间相差远小于5%,完全能够替代目前地震台使用的RN-150型氡源,同时具有操作简便、体积小、易携带等优点。 相似文献