基于IRS-P5卫星立体影像的地形图测绘试验   总被引：1，自引：0，他引：1  

赵巍  杨静  王海燕  李英利  闫会杰  蒙晓峰 《测绘标准化》2008,(2):34-38

简要介绍了印度 IRS-P5卫星立体影像的特点及其应用前景,重点介绍了使用某地区的立体像对数据进行的1:10000地形图测绘有关试验研究。结果表明,在高精度的地面控制点的支持下,地形类别为山地的地形图平面和高程精度均可满足国家1:10000基本比例尺地形图测图规范要求。  相似文献   

中国西南地区二叠纪乐平世陆生生物大灭绝期煤中砷和硒的演化及古环境意义   总被引：1，自引：1，他引：0       下载免费PDF全文

雒昆利  李会杰  牛彩香  陈同斌 《古地理学报》2008,10(4):385-394

为了探讨中国西南地区二叠系乐平统(上二叠统)龙潭组中下部煤系不同煤组分中砷、硒的含量和演化及古环境意义,对近10年来采集于中国西南扬子地台的二叠系乐平统龙潭组主采煤层的原煤、亮煤、煤矸石、黄铁矿结核等样品中砷、硒元素含量进行了测定和分析,并与中国华北地台一些煤矿的上石炭统-下二叠统太原组、山西组的原煤、镜煤、亮煤、煤矸石、黄铁矿结核等样品中砷、硒含量进行对比分析。结果表明：西南地区乐平统龙潭组煤的砷、硒含量变化较大,但总体高于华北晚石炭世和早二叠世煤的砷、硒含量;西南二叠系乐平统龙潭组大多数的亮煤中砷、硒含量高于原煤全煤样(刻槽样)中的砷、硒含量,也远远高于同煤层煤矸石的含量,龙潭组部分亮煤的砷含量尤其高,为55～338 mg/kg,还发现砷含量为89 mg/kg的亮煤。但华北上石炭统-下二叠统的镜煤中的砷、硒含量与之相反,低于原煤全煤样的砷、硒含量,其中砷含量非常低,为063～129 mg/kg。说明西南地区上二叠统煤中的砷和硒与煤的有机质密切相关,可能主要来源于成煤古植物。在西南乐平世早、中期第Ⅰ幕陆生生物集群灭绝事件期间,陆生动物的食物--植物中有毒有害元素砷、硒含量明显增加,陆生环境或泥炭沼泽中可溶性砷、硒含量增加。  相似文献   

禹州煤田泉店井田构造特征及对其二1煤层的影响     

张云中姜敏德  李惠杰田张丽 《中国煤田地质》2005,17(5):8-10

对泉店井田的地质构造进行了分析研究,阐明了断层及褶曲的分布,探讨了井田的构造演化,分析了构造特别是断层对二1煤层的影响,为今后煤矿开发生产提供了可靠的地质依据.  相似文献   

Water mining from the deep critical zone by apple trees growing on loess     

Huijie Li  Bingcheng Si  Pute Wu  Jeffrey J. McDonnell 《水文研究》2019,33(2):320-327

There have been significant recent advances in understanding the ecohydrology of deep soil. However, the links between root development and water usage in the deep critical zone remains poorly understood. To clarify the interaction between water use and root development in deep soil, we investigated soil water and root profiles beyond maximum rooting depth in five apple orchards planted on farmland with stand ages of 8, 11, 15, 18, and 22 years in a subhumid region on the Chinese Loess Plateau. Apple trees rooted progressively deeper for water with increasing stand age and reached 23.2 ± 0.8 m for the 22‐year‐old trees. Soil water deficit in deep soil increased with tree age and was 1,530 ± 43 mm for a stand age of 22 years. Measured root deepening rate was far great than the reported pore water velocity, which demonstrated that trees are mining resident old water. The deficits are not replenished during the life‐span of the orchard, showing a one‐way mining of the critical zone water. The one‐way root water mining may have changed the fine root profile from an exponential pattern in the 8‐year‐old orchard to a relative uniform distribution in older orchards. Our findings enhance our understanding of water‐root interaction in deep soil and reveal the unintended consequences of critical zone dewatering during the lifespan of apple trees.  相似文献   

Energy budgets on the interactions between the mean and eddy flows during a persistent heavy rainfall event over the Yangtze River valley in summer 2010   总被引：1，自引：1，他引：0       下载免费PDF全文

傅慎明  汪汇洁  孙建华  张元春 《Acta Meteorologica Sinica》2016,30(4):513-527

In this study,a persistent heavy rainfall event(PHRE) that lasted for around 9 days(from 0000 UTC 17 to0000 UTC 26 June 2010) and caused accumulated precipitation above 600 mm over the Yangtze River valley,was reasonably reproduced by the advanced research WRF model.Based on the simulation,a set of energy budget equations that divided the real meteorological field into the mean and eddy flows were calculated so as to understand the interactions between the precipitation-related eddy flows and their background circulations(BCs).The results indicated that the precipitation-related eddy flows interacted with their BCs intensely during the PHRE.At different layers,the energy cycles showed distinct characteristics.In the upper troposphere,downscaled energy cascade processes appeared,which favored the maintenance of upper-level eddy flows;whereas,a baroclinic energy conversion,which reduced the upper-level jet,also occurred.In the middle troposphere,significant upscaled energy cascade processes,which reflect the eddy flows’ reactionary effects on their BCs,appeared.These effects cannot be ignored with respect to the BCs’ evolution,and the reactionary effects were stronger in the dynamical field than in the thermodynamical field.In the lower troposphere,a long-lived quasi-stationary lower-level shear line was the direct trigger for the PHRE.The corresponding eddy flows were sustained mainly through the baroclinic energy conversion associated with convection activities.Alongside this,the downscaled energy cascade processes of kinetic energy,which reflect the direct influences of BCs on the precipitation-related eddy flows,were also favorable.A downscaled energy cascade of exergy also appeared in the lower troposphere,which favored the precipitation-related eddy flow indirectly via the baroclinic energy conversion.  相似文献   

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李德前  陈慧杰  魏贵春  孙伶俐  戴苗  贺玉方 《大地测量与地球动力学》2015,35(2):356-359

??????????????????????????????????????????????????????в?????????????????????????????????????????????≤1 nT/m????????????≤0.1 nT?????????????????????????????????????????????????????в???????????????????????????????????  相似文献   

浅议矿业权转让市场建设与地勘行业改革的关系     

蒋辉杰 《青海国土经略》2001,(1)

笔者从地勘单位由事转企改革的角度,分析论证矿业权转让市场建设的迫切性,并对矿业权转让市场建设中有关的交易对象、矿业权价值认定、矿业权利益取得以及市场的启动与运作等问题,提出了一些具体的意见,使该市场真正对地勘改革和社会主义市场经济建设起到积极地促进作用。  相似文献   

基于无人机遥感和面向对象法的简单地物分类研究     

袁慧洁 《测绘与空间地理信息》2020,(3):113-117,123

近年来,全国各地进行了大范围的土地利用调查,随着无人机遥感技术越来越成熟,无人机影像分析技术已深入应用到土地利用调查中,其中最多的用途是地物分类。本文选择昭通市昭阳区某乡镇区域为研究区,对采集到的无人机影像进行预处理,生成对应的正射影像;基于多种可见光植被指数,计算每3种指数合并得到影像的OIF指数,确定最佳波段组合;采用基于规则和基于样本两种面向对象分类方法,提取房屋、道路、植被等简单地物及背景。分析结果:两种方法的提取精度均达到90%以上,基于规则的面向对象分类方法精度较高,但耗时较长;基于样本的面向对象方法耗时较短,精度相对较低。两种方法相结合的全自动分类提取是下一步研究的目标。  相似文献   

Remote sensing linear trends of the Gulf Stream from 1993 to 2016     

Zhang  Wen-Zhou  Chai  Fei  Xue  Huijie  Oey  Lie-Yauw 《Ocean Dynamics》2020,70(5):701-712

Ocean Dynamics - The Gulf Stream (GS) transports a massive amount of heat northward to high latitudes and releases sensible and latent heat to the atmosphere, playing an important role in the North...  相似文献   

A model study of the Copper River plume and its effects on the northern Gulf of Alaska     

Yuan Wang  Huijie Xue  Fei Chai  Yi Chao  John Farrara 《Ocean Dynamics》2014,64(2):241-258

A three-level nested Regional Ocean Modeling System was used to examine the seasonal evolution of the Copper River (CR) plume and how it influences the along- and across-shore transport in the northern Gulf of Alaska (NGoA). A passive tracer was introduced in the model to delineate the growth and decay of the plume and to diagnose the spread of the CR discharge in the shelf, into Prince William Sound (PWS) and offshore. Furthermore, a model experiment with doubled discharge was conducted to investigate potential impacts of accelerated glacier melt in future climate scenarios. The 2010 and 2011 simulation revealed that the upstream (eastward) transport in the NGoA is negligible. About 60 % of the passive tracer released in the CR discharge is transported southwestward on the shelf, while another one third goes into PWS with close to 60 % of which exiting PWS to the shelf from Montague Strait. The rest few percent is transported across the shelf break and exported to the GoA basin. The downstream transport and the transport into PWS are strongly regulated by the downwelling-favorable wind, while the offshore transport is related to the accumulation of plume water in the shelf, frontal instability, and the Alaskan Stream. It takes weeks in spring for the buoyancy to accumulate so that a bulge forms outside of the CR estuary. The absence of strong storms as in the summer of 2010 allows the bulge continue growing to trigger frontal instability. These frontal features can interact with the Alaskan Stream to induce transport pulses across the shelf break. Alternatively as in 2011, a downwelling-favorable wind event in early August (near the peak discharge) accelerates the southwestward coastal current and produces an intense downstream transport event. Both processes result in fast drains of the buoyancy and the plume content, thereby rapid disintegration of the plume in the shelf. The plume in the doubled discharge case can be two to three times in size, which affects not only the magnitude but also the timing of certain transport events. In particular, the offshore transport increases by several folds because the plume appears to be more easily entrained by the seaward flow along the side of Hinchinbrook Canyon.  相似文献