基于遗传算法的东湖水质参数反演方法探讨   总被引：1，自引：0，他引：1  

高铎  方圣辉  张雪虎  罗莎  梁静 《测绘信息与工程》2006,31(6):42-44

引入了叶绿素浓度的对数和浊度的对数作为变量,建立了前向光学模型和遗传算法的目标函数,实现了较高的反演精度。  相似文献   

西藏羊八井地热田热水的化学组成   总被引：12，自引：0，他引：12       下载免费PDF全文

赵平  多吉 《地质科学》1998,33(1):61-72

羊八井地热田深、浅层热水都是Cl-Na类型,具有相同的B/Cl比值,说明深层热水在上升通道中与冷水相混合形成了浅层热水。浅层流体自西北向东南流动,温度逐渐降低。浅层热储内普遍存在着水岩交换反应,对热水的化学组成有一定的影响。石英和玉髓地热温度计分别适用于计算深、浅层的热储温度。纳木错(湖)不是羊八井地热田的补给区。深层热水在井筒内绝热汽化时不会出现SiO₂结垢,CaCO₃是否会在井筒壁沉淀需要放喷较长时间来检验。文中还阐述了对热水的化学组分进行监测的必要性。  相似文献   

流域地貌系统定量研究的新指标   总被引：6，自引：3，他引：3  

王协康  方铎 《山地学报》1998,(1)

简要介绍了分形基本理论,着重讨论了流域地貌系统定量研究的指标．水系分维的计算方法,水系分维区域划分原则及其应用含义．  相似文献   

Sequence Boundary and Sea Level Changes in Western Margin of Upper Yangtze Platform during Permian and Triassic     

Xu Xiaosong Liu Baojun Zhao Yuguang 《中国地质大学学报(英文版)》1996,(1)

TECTONICac~ac~~RA~m~NERGoorU~YANG~~oafNdsreof~actTheho~ofUPperYangtzePlatformwascpetallizedandconsolidatedinthekiaogUanhernovernentofMeSoproterocoic(ca.1700mp.ItconstituteSthestableCentralSichuanconiinelhalnucleusandthecratonakin.Therearetabtabofcontinental~ionsurroUndingtheCentralSichuanconti~alnuCleusduring1700--800the.ThebordersofthecontinentalaCCretionareconcordantacthebordersof~nicandPalcogngnphy,andalsofo~theboundarybet~basin~formationS.InPaloocoic,tab~nicCycleScormspond…  相似文献   

近百年长江下游作物生长季冷暖的变化与大型环流的振动   总被引：2，自引：1，他引：2  

汪铎  张镡 《气象学报》1989,47(3):287-295

本文运用上海1373—1982年110年气温资料,配合1871—1980年110年月平均海平面气压场资料,分析了长江下游作物生长季冷暖的长期变化以及与之关联的大型环流变化特征。发现最近百余年里,年、季(代表月份)和关键旬的平均气温普遍经历了从偏冷期转为偏暖期约80—100年周期的振动,转折发生在本世纪20年代末、30年代初。70年代前后有转向偏冷期的趋势。这类低频振动与大型环流活动的低频振动有密切关联,主要表现在冬季亚洲大陆冷高压主体偏东和阿留申低压偏弱时期,相应夏季青藏高原热低压偏弱时期,对应长江下游偏冷期;反之,则对应偏暖期。讨论了生长季冷暖变化对农作物生长发育和产量的影响。  相似文献   

The band characteristics of long-term variation of precipitation and water resources in east asia monsoon region     

Wang Duo  Zhang Tan 《大气科学进展》1989,6(3):347-356

In this paper, by means of the “CWH” (circulation-weather and climate-agricultural harvest) analytical meth-od, drawing from the monthly mean long-term data of the global sea level pressure field and annual precipitation data and grain yield data of some regions in East Asia, the time-space characters of low-frequency fluctuation of East Asian precipitation with band distribution are analyzed.It is revealed that the band of 20-30 years quasi-periodic fluctuation is located in Southeast Asia and the coastal areas of South China. Moving forward to west and north, the period of fluctuation of precipitation tends to become longer, both bands, with about 40-yr and 60-80-yr quasi-periodic fluctuation are respectively situated in the middle-lower reaches of the Yangtze River and North or Southwest China. Furthermore, the relationships between the fluctuations of precipitation bands and large-scale circulations are analyzed. The relationships between precipita-tion and types of water resources are discussed as well. In addition, the tendency of long-term variation in rainfall is predicted.  相似文献   

川滇黔桂地区志留纪构造－岩相古地理   总被引：19，自引：5，他引：19       下载免费PDF全文

万方  许效松 《古地理学报》2003,5(2):180-186

晚奥陶世与早志留世之间的都匀运动，使滇中古隆起与黔中古隆起成为一整体隆起带（习惯上称黔中古陆），把滇东南和黔南与滇东北-黔北-川南分隔为南、北两个不同的构造沉积域。南侧的曲靖一带出露下、中寒武统，其上分别与中、上志留统和下泥盆统呈假整合，其间缺失奥陶纪和早志留世的沉积物。北侧的禄劝－武定一带，下古生界的沉积序列与之相反，有完整的奥陶纪沉积组合，上与泥盆系假整合，其间无志留纪的沉积。这表明黔中古陆两侧的沉积域各为独立的系统。中晚志留世，黔中古隆起南侧应归属于上扬子与滇黔桂地块前陆挠曲盆地的一部分，由曲靖向北东经赫章哑都-贵阳南转向湘西，向南则与云南的绿春海相连，黔中古隆起北侧的沉积域则为上扬子前陆（川南-黔北）盆地的边缘相。  相似文献   

沿河县地质灾害特征、成因及防治   总被引：1，自引：0，他引：1  

舒多友 《贵州地质》2003,20(3):172-177

本文对贵州省沿河县地质灾害的地质背景进行了调查研究，指出了该县地质灾害的特征和成因及其防治途径。  相似文献   

Partial Melting and Its Implications for Understanding the Seismic Velocity Structure within the Southern Tibetan Crust   总被引：2，自引：0，他引：2  

YANG Xiaosong  MA Jin  JIN Zhenmin  GAO Shan  MA Shengli Geology Institute  China Seismological Bureau  Beijing  Laboratory of Tectonophysics  China Seismological Bureau  Beijing Faculty of Earth Sciences  China University of Geosciences  Wuhan  Hubei 《《地质学报》英文版》2003,77(1):64-71

In order to constrain the crustal wave velocity structure in the southern Tibetan crust and provide insight into the contribution of crustal composition, geothermal gradient and partial melting to the velocity structure, which is characterized by low average crustal velocities and widespread presence of low-velocity zone(s), the authors model the crustal velocity and density as functions of depth corresponding to various heat flow values in light of velocity measurements at high temperature and high pressure. The modeled velocity and density are regarded as comparison standards. The comparison of the standards with seismic observations in southern Tibet implies that the predominantly felsic composition at high heat flow cannot explain the observed velocity structure there. Hence, the authors are in favor of attributing low average crustal velocities and low-velocity zone(s) observed in southern Tibet mainly to partial melting. Modeling based on the experimental results suggests that a melting percentage  相似文献   

Progress and prospects of applied research on physical geography and the living environment in China over the past 70 years (1949–2019)   总被引：2，自引：1，他引：1  

Chen  Fahu  Wu  Shaohong  Cui  Peng  Cai  Yunlong  Zhang  Yili  Yin  Yunhe  Liu  Guobin  Ouyang  Zhu  Ma  Wei  Yang  Linsheng  Wu  Duo  Lei  Jiaqiang  Zhang  Guoyou  Zou  Xueyong  Chen  Xiaoqing  Tan  Minghong  Wang  Xunming  Bao  Anming  Cheng  Weixin  Dang  Xiaohu  Wei  Binggan  Wang  Guoliang  Wang  Wuyi  Zhang  Xingquan  Liu  Xiaochen  Li  Shengyu 《地理学报(英文版)》2021,31(1):3-45

Physical geography is a basic research subject of natural sciences.Its research object is the natural environment which is closely related to human living and development,and China's natural environment is complex and diverse.According to national needs and regional development,physical geographers have achieved remarkable achievements in applied basis and applied research,which also has substantially contributed to the planning of national economic growth and social development,the protection of macro ecosystems and resources,and sustainable regional development.This study summarized the practice and application of physical geography in China over the past 70 years in the following fields:regional differences in natural environments and physical regionalization;land use and land cover changes;natural hazards and risk reduction;process and prevention of desertification;upgrading of medium-and low-yield fields in the Huang-Huai-Hai region;engineering construction in permafrost areas; geochemical element anomalies and the prevention and control of endemic diseases;positioning and observation of hysical geographical elements;and identification of geospatial differentiation and geographical detectors. Furthermore, we have proposed the future direction of applied research in the field of physical geography.  相似文献