Geomorphic Evidence for and Rate of Sinistral Strike-slip Movement Along Northwest-trending Faults in Chaoshan Plain     

Wang Yipeng  Song Fangmin  Huang Qingtuan  Chen Weiguang 《中国地震研究》2000,14(4):357-366

Two sets of active faults,northwest-and northeast-trending faults,are developed in the Chao-shan Plain of East Guangdong.After detailed interpretation of aerophotos,we have found outthat there is the clear phenomenon of sinistral dislocation of drainage system on the Huang-gang-shui fault and part of Fengshun-Shantou fault.Field investigation confirmed that the geo-morphic bodies along the two faults have undergone displacement.Large-scale topographicmapping was made at three displaced sites and samples for age dating were collected from thegeomorphic booies.Calculation indicates that the average rate of sinistral strike-slip movementin the Holocene time amounts to 1.11±0.09～2.69±0.24mm/a along the Huanggangshuifault and 3.26±0.26mm/a along the Fengshun-Shantou fault.These two more active NW-trending faults extend into sea area,where they intersect the NE-trending strongly active Nius-han Island-Xiongdi Isle-Nanpeng Isles fault at a depth of 40～50m in water.The intersection isa location favorable fo  相似文献   

包气带水气二相流国外研究综述   总被引：3，自引：0，他引：3  

彭胜  陈家军  王金生  王志明  李书绅 《水科学进展》2000,11(3):333-338

与传统的包气带中水流研究相比,水气二相流更准确地描述了包气带中的水与空气的流动情况,这对更好地了解固体废物处置场中污染物的运动规律具有重要的意义.与一相流明显不同的是,二相流考虑了空气的运动及其对水流的作用.根据国外近几十年来不同研究者的研究结果,总结了入渗过程中水的流动、空气对水流的影响及空气本身的压力变化情况,并分析了不同作者研究结果的差别.  相似文献   

洞穴石笋沉积速率研究中值得注意的几个问题   总被引：12，自引：5，他引：7  

林玉石  张美良  覃嘉铭 《中国岩溶》2001,20(2):131-136

众多大型石笋纵剖面观测、测年和纹层沉积计率(沉积速率计算)表明,速率差异是石笋沉积特征的重要数据,也是古气候环变化的重要反映,但以往诸多资料不好引用、无从对比。通过筛选石笋的全(正)心纵剖面,沿纹层轴(中)部采样,测年值和计率可信度大,具时空对比意义。为提高精度和分辨率,提倡按石笋沉积特征段,特别是纹层组测年计率。   相似文献   

沙冬青对土壤水分变化的生理响应   总被引：40，自引：17，他引：23  

冯金朝  周宜君  周海燕  张景光 《中国沙漠》2001,21(3):223-226

沙冬青(Ammopiptanthus mongolicus(Maxim))是生长在沙漠地区及干旱荒漠区的常绿灌木,在干旱环境条件下形成了独特的生物学特性与生理生态适应性。研究结果表明,灌水前后沙冬青的光合作用和蒸腾作用变化很大。在土壤干旱时,其光合速率变化的日平均值仅为2.14μmol·m^-2·s^-1,其最大值仅为3.5μmol·m^-2·s^-1;此时叶片蒸腾速率变化的日平均值为7.03mmol·m^-2·s^-1,最大值为10.5mmol·m^-2·s^-1。而在土壤水分充足时,其光合强度和蒸腾强度明显提高,叶片光合速率的日平均值为5.97μmol·m^-2·s^-1,最大值为8.5μmol·m^-2·s^-1,均为干旱时的2倍以上;此时叶片蒸腾速率的日平均值为23.5mmol·m^-2·s^-1,最高值达30.1mmol·m^-2·s^-1,均为干旱时的3倍左右。分析沙冬青叶片气孔的调节作用与叶片的光合作用和蒸腾作用的关系可知,其气孔活动与蒸腾作用保持较为密切的相关关系,而其光合作用虽然也受气孔活动的影响,更主要是与其自身的生理生化特性有关。  相似文献   

润扬大桥北锚碇岩石流变特性的试验研究   总被引：13，自引：3，他引：10  

赵永辉  何之民  沈明荣 《岩土力学》2003,24(4):583-586

为了解润扬长江大桥北锚基础岩石的流变力学特性,针对北锚基础区域的岩样,通过模拟其受力的实际情况,采用岩石双轴流变试验机进行了单轴压缩蠕变试验,并选用广义的Kelvin模型进行了参数拟合分析,掌握了岩石蠕变的基本规律,并获得了粘滞系数等相关的流变力学参数。  相似文献   

中国气候雪线空间分布特征   总被引：5，自引：3，他引：2  

蒋复初  吴锡浩  王书兵  傅建利 《地质力学学报》2002,8(4):289-296

气候雪线的空间分布规律既受高度地带性和纬度地带性限制,也受区域性气候的控制。雪线空间格局变化实质上是水热条件变化的反映。本文主要依据我国106个气象站的气象资料,从年均温、年降水量和固态降水率之间的相关函数计算出气候雪线高程,进而探讨中国大陆气候雪线的空间分布特征。   相似文献   

科尔沁沙地奈曼旗近5年来风况及合成输沙势   总被引：21，自引：13，他引：8  

张华  李锋瑞  李玉霖  伏乾科 《中国沙漠》2004,24(5):623-627

应用奈曼沙漠化研究站1998-2002年的气象资料, 统计分析了奈曼旗近5a来的风况特征和输沙势。结果表明: ①研究区3~5月起沙风发生频数最高, 占全年起沙风的38%~58%; 平均风速和最大风速值最大, 分别为6.0~7.5m·s^-1和9.5~16.9m·s^-1。该风况特征与地表冻融、裸露、干旱疏松相耦合, 形成了区内的风沙活动期。②在风沙活动期内, 风环境基本为锐双峰风况, 西北风居主导地位, 频数占54%; 南风和西南风次之, 频数占38%。③在风沙活动期内, 研究区属于高风能环境, 合成输沙势RDP为66.3VU(风速以m·s^-1为单位), 合成输沙方向RDD为ESE113°。  相似文献   

Local Similarity Relationships of Non-Dimensional Wind and Temperature Gradient in the Tower-Layer Atmosphere over Beijing City     

Al-Jiboori M. H.  Xu Yumao  Qian Yongfu 《大气科学进展》2000,17(4):636-648

Micrometeorological data for wind and temperature from a 325 m high tower in Beijing City are analyzed by use of local similarity theory. Non-dimensional wind and temperature gradients, Фm and Фh, are determined by three techniques called, respectively, eddy-correlation, mean profiles and inertia-subrange cospectra (ISC) method for a wide range of atmospheric stratification from unstable to stable conditions. Average dissipation rate Фε of turbulent kinetic energy (TKE) is evaluated from u-spectrum, as a quantity required in the last technique. Ratio of the eddy transfer coefficients. α (= Kh / Km,), is calculated from Фm and Фh estimations. The results from various techniques are compared with each other and with some available empirical results in the tower-layer. It is shown that the empirical relationships determined by mean profiles and ISC methods in the tower-layer turbulence are in agreement with each other and with some other results.  相似文献   

    

Al-Jiboori M. H.  Xu Yumao  Qian Yongfu 《大气科学进展》2000,17(4):636-648

Micrometeorological data for wind and temperature from a 325 m high lower in Beijing City are analyzed by use of local similarty theory Non–dimentional wind and temperature gradients Φ and Φ are determined by three techniques called respectively, eddy-correlation, mean profiles and inertia subrange cospectra (ISC) method for a wide range of atmospheric stratification from unstable to stable condition Average dissipation rate Φof turbulent kinetic energy (TKE) is evaluated from u-spectrum as a quanlity required in the last technique. Ratio of the eddy transfer coefficients. α(= K / K) is calculated from Φ and Φ estimations. The results from various techniques are compared with each other and with some available empirical results in the lwor -layer. it is shown that the empirical relationship detefrmined by mean profiles and ISC methods in the lower-layer turbulence are in agreement with each other and with some other results. Supported by the National Natural Science Foundation of China under Grant No.49735170. The authors are very grateful to the members, working for the State Key Lab. of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, the Institute of Atmospheric Physics in Beijing, who supplied the data from the meteorological tower for this paper. The authors wish to thank to Mrs. Israa H. A. in the presentation of data on the required style.  相似文献   

Late Cenozoic Tectonics Along the Northwestern Margin of the Tarim Basin: Interactions Between the Tarim Basin and the Southern Tian Shan, West China     

Chen Jie  Qu Guosheng  Shen Jun  Edward Sobel  Nan Ling  Tian Qinjian  Yin Jinhui 《地学前缘》2000,(Z1)

LATE CENOZOIC TECTONICS ALONG THE NORTHWESTERN MARGIN OF THE TARIM BASIN: INTERACTIONS BETWEEN THE TARIM BASIN AND THE SOUTHERN TIAN SHAN, WEST CHINAgrants 4 98340 50and 4 9732 0 90fromtheNSFofChina;;andproject96 913 0 7 0 1fromtheMinistryofSci enceandTechnology ,China…  相似文献