巴颜喀拉山地区第四纪冰期初步探讨     

朱建立 《青海国土经略》1992,(2)

依据地貌、孢粉、岩性沉积特征,划分巴颜喀拉山地区第四纪冰期。并与珠穆朗玛峰、唐古拉山、昆仑山地区进行对比。确定巴颜喀拉山地区第四纪以来有:哈拉滩冰期;巴颜喀拉山冰期;洛曲冰期;汪藏因姆措冰期;折尕考钦新冰期。  相似文献   

1988年1月云南威信墨黑山地灾害     

吴其伟  李德基  朱平一  冯水志 《山地学报》1988,(3)

这次山地灾害由岩崩、滑坡和泥石流三类灾害组成。在我国西南,隆冬少雨季节出现这类山地灾害是罕见的。这次山地灾害正是发生于1988年1月,具有一定的特殊性。究其原因是,当地某些较为特殊的自然条件和采煤不当,促使山体岩崩崩积物逐年加载,进而引起滑坡、泥石流的发生。灾害造成的直接经济损失合人民币58.6万元。对此种山地灾害宜采取以避害为主的防治措施。  相似文献   

Jordan日照记录阈值分析     

Li Jiarui Qian Daojun Zhu Huaming 《成都信息工程学院学报》1989,(1)

本文是通过10个月的日射、日照资料对比观测、统计的乔唐、康氏和光电式日照计记录阈值的平均值和标准偏差,分析了乔唐日照计进光孔径、涂药方式对感光迹线的影响,测定了感光药的吸收光谱,并根据日出日没时直接日射辐照度的平均变化率,估算了由阈值的不确定度引起的日照时数的误差,从而为我国几十年的乔唐日照资料的评价提供依据。  相似文献   

The distribution and natural degradation of cyanide in goldmine tailings and polluted soil in arid and semiarid areas   总被引：2，自引：0，他引：2  

Li Shehong  Zheng Baoshan  Zhu Jianming  Yu xiaoying 《Environmental Geology》2005,47(8):1150-1154

Farmlands and rivers have been seriously polluted by cyanide from a goldmine tailings dam that collapsed in early spring of 1995 in Yining County, Xinjiang Autonomous Region of China. The cyanide distribution in the polluted farmland and the abandoned tailings dam was studied, three and 4 years after the accident occurred. The results indicated that natural degradation of cyanide in soils is slower than in natural water bodies. The cyanide transport in the soil section is similar to freely soluble salts. In arid and semiarid areas, cyanide can be highly enriched in the salt crust in which the concentration is even higher than the fresh tailings debris though cyanide has decomposed for 4 years. In the polluted farmland, the sticky layer in the soil section can highly adsorb and enrich cyanide so it can partly prevent cyanide transfer to groundwater. According to the characteristics of cyanide natural degradation in soil, the measures for prevention and cure of soil polluted by goldmine tailing dam collapse have been discussed.  相似文献   

S-wave velocity and Poisson''''s ratio structure of crust in Yunnan and its implication   总被引：13，自引：2，他引：11  

HU Jiafu  SU Youjin  ZHU Xiongguan & CHEN Yun Geophysical Department of Yunnan University  Kunming  China  Seismological Bureau of Yunnan Province  Kunming  China  Institute of Geology  Geophysics  Chinese Academy of Sciences  Beijing  China 《中国科学D辑(英文版)》2005,48(2):210-218

Receiver function of body wave under the 23 stations in Yunnan was extracted from 3-component broadband digital recording of teleseismic event. Thus, the S-wave velocity structure and distribution characteristics of Poisson's ratio in crust of Yunnan are obtained by inversion. The results show that the crustal thickness is gradually thinned from north to south. The crustal thickness in Zhongdian of northwest reaches as many as 62.0 km and the one in Jinghong of further south end is only 30.2 km. What should be especially noted is that there exists a Moho upheaval running in NS in the Chuxiong region and a Moho concave is generally parallel to it in Dongchuan. In addition, there exists an obvious transversal inhomogeneity for the S-wave velocity structure in upper mantle and crust in the Yunnan region. The low velocity layer exists not only in 10.0-15.0 km in upper crust in some regions, but also in 30.0-40.0 km in lower crust. Generally, the Poisson's ratio is on the high side, however it has a better co  相似文献   

Climatological distribution of lightning density observed by satellites in China and its circumjacent regions   总被引：14，自引：1，他引：13  

MA Ming  TAO Shanchang  ZHU Baoyou & LU Weitao School of Earth  Space Sciences  University of Science  Technology of China  Hefei  China 《中国科学D辑(英文版)》2005,48(2):219-229

The 0.5°×0.5°grid resolution distribution of lightning density in China and its circumjacent regions have been analyzed by using the satellite-borne OTD (Apr 1995-Mar 2000) and LIS (Dec 1997-Mar 2003) databases. It is shown that: (i) Firstly, the variability of the lightning density (LD) is particularly pronounced over the different subareas, 9 times greater over the south than the north side of Himalayas Mountains, 2.5 times greater over the eastern than the western area of China. While the maximum and minimum LD are respectively 31.4fl/km2/a (in Guangzhou region) and less than 0.2fl/km2/a (in the desert of western China). Secondly, the LD of China's continent regularly varies with latitude and distance off coast, which is consistent with annual mean precipitation in varying trend. In conclusion, the Qinghai-Tibet Plateau, the China's three-step staircase topography and the latitude are three important factors affecting macro-scale characteristics of the LD distribution, (ii) The regional differences  相似文献   

Cataclastic rheology of carbonate rocks     

LU Xiancai  SUN Yan  SHU Liangshu  GU Lianxing  GUO Jichun & ZHU Wenbin State Key Laboratory of Mineral Deposits Research  Department of Earth Sciences  Nanjing University  Nanjing  China 《中国科学D辑(英文版)》2005,48(8):1227-1233

  相似文献   

Adjoint method for the optimum planning of industrial pollutant sources     

LIU Feng    HU Fei & ZHU Jiang . College of Environmental Sciences  Peking University  Beijing  China  . LAPC  Institute of Atmospheric Physics  Chinese Academy of Sciences  Beijing  China 《中国科学D辑(英文版)》2005,48(8):1270-1279

The deterioration of air quality is threatening the life and health of people. Scientists in China and other countries have done a great deal of research work on the details of air pollution and the methods of preven-tion and control during the past decades. Up to now, most of the achievements are concentrated on the techniques of controlling pollutant sources and the programs of reduction, which focus on the improve-ment of air quality and the restoration of environment. The techniques of con…  相似文献   

On the problem of land melioration on the Chinese Loess Plateau     

Xian-mo Zhu  S. M. Chu 《GeoJournal》1995,36(2-3):289-294

The Loess Plateau in Northwestern China, with 60 million inhabitants, is strongly endangered by heavy erosion quickly decreasing soil fertility and yield of crops, causing also severe problems in the main river of the area, uplifting its bed by strong sedimentation. This situation is mainly due to improper land use, cutting woods, ploughing up grasslands which are the consequence of the decreasing yield of former plough lands. This vicious cycle may only be disrupted by a proper land management based on the newest results of scientific research, on up to date data bases as well as on traditional methods. The land melioration methods must primarily aim at a prevention of further erosion and at an increase of infiltration by different methods, but all means of a proper country planning and development should be harmonised in order of halting of further deterioration of the area.  相似文献   

中天山坡地冰缘地貌的若干问题   总被引：1，自引：0，他引：1  

朱诚 《山地学报》1992,(2)

由 1985—1989年野外调查结果和定位重复观测资料可知,本区坡地冰缘地貌的分布特征为:1.各类坡地冰缘形态彼此具有成因联系;2.不同序次的冰缘地貌类型具有各自的时空分异;3.不同的坡地冰缘地貌类型在一定条件下可有所转化。再则,本区风化以寒冻剥裂和寒冻楔入为主,呈现在时空和状态上为不可逆过程的耗散结构。  相似文献