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库姆塔格沙漠“羽毛状沙丘”形态的示量特征 被引量:19
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作者 刘虎俊 王继和 +8 位作者 廖空太 郑庆中 张锦春 丁峰 唐进年 俄有浩 苏志珠 翟新伟 张国忠 《干旱区地理》 CSCD 北大核心 2006年第3期314-320,共7页
通过卫星照片判读和实地观测,库姆塔格沙漠的“羽毛状沙丘”由两种风沙地貌构成:东北-西南走向的新月形“沙垄”为“羽轴”;垄间分布的波状微起伏的“大沙波”为“羽枝”,“大沙波”与沙垄的夹角为75°~103°。二者组合成类... 通过卫星照片判读和实地观测,库姆塔格沙漠的“羽毛状沙丘”由两种风沙地貌构成:东北-西南走向的新月形“沙垄”为“羽轴”;垄间分布的波状微起伏的“大沙波”为“羽枝”,“大沙波”与沙垄的夹角为75°~103°。二者组合成类似“羽毛”的风沙地貌。新月形“沙垄”由单个新月形沙丘的前一沙丘的迎风坡与后一沙丘东翼相连构成“沙垄”。组成“沙垄”的新月形沙丘的两翼平均长37.5m,翼间距30~66m,沙丘高3~19m;在所观测区域内,沙丘沙的分选性由南向北变差。新月形“沙垄”长为3~22km,垄间距为1~3km,其问分布浅色和暗色相间的波状微地貌,暗色部分平均宽24.3m,浅色部分的平均宽11.6m。暗色部分表层沙粒的粒径有60%在1.00~0.25mm之间,以暗色矿物为主,而浅色部分表层沙粒的粒径的90%在1.00~0.25mm之间,分选性相对暗色部分较好,以石英等浅色矿物为主。暗色和浅色微地貌成对出现,相对高差约7cm。这种波状微地貌在库姆塔格沙漠中北部重复出现,类似于风沙地貌分类的沙波,暂称其为“大沙波”。 展开更多
关键词 库姆塔沙漠 “羽毛状沙丘” 示量
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库姆塔格沙漠的“羽毛状沙丘”形态的观测 被引量:10
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作者 刘虎俊 王继和 +8 位作者 廖空太 郑庆钟 张锦春 丁峰 唐进年 俄有浩 苏志珠 张国中 翟新伟 《地学前缘》 EI CAS CSCD 北大核心 2007年第3期190-196,共7页
参照卫星照片和地形图,实地观测了库姆塔格沙漠“羽毛状沙丘”分布区域的地貌。新月型“沙垄”是该区域的主导性地貌类型,垄间地形波状起伏。如果将“沙垄”喻为“羽轴”,垄间的波状起伏地形为“羽枝”,则可构成卫星照片所显示的“... 参照卫星照片和地形图,实地观测了库姆塔格沙漠“羽毛状沙丘”分布区域的地貌。新月型“沙垄”是该区域的主导性地貌类型,垄间地形波状起伏。如果将“沙垄”喻为“羽轴”,垄间的波状起伏地形为“羽枝”,则可构成卫星照片所显示的“羽毛状沙丘”。新月型“沙垄”的走向为NE-SW,由新月形沙丘前一沙丘的迎风坡与后一沙丘的东翼相连而成,高3~19m,宽约50m,长15-22km。“垄”间起伏地形的波长为100-300m,振幅为40~100cm,与“沙垄”成60-105°夹角。在波状起伏地形的波峰与波谷过渡区堆积颜色较浅的细沙,厚2~7cm,构成了“大沙波”。实地观测的“羽毛状沙丘”的形态与卫星照片显示的形态有一定差异。 展开更多
关键词 库姆塔格沙漠 “羽毛状沙丘” 形态
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关于库姆塔格沙漠“羽毛状”风沙地貌的讨论 被引量:22
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作者 董治宝 屈建军 +1 位作者 卢琦 钱广强 《中国沙漠》 CSCD 北大核心 2008年第6期1005-1010,1214,共7页
库姆塔格沙漠是我国最后一个完成综合科考的沙漠,以其北部的"羽毛状"沙丘著称。以往关于库姆塔格沙漠风沙地貌的认识主要基于遥感影像判读。最近深入沙漠腹地的实地考察引发了对该沙漠"羽毛状"沙丘的争论。本文从... 库姆塔格沙漠是我国最后一个完成综合科考的沙漠,以其北部的"羽毛状"沙丘著称。以往关于库姆塔格沙漠风沙地貌的认识主要基于遥感影像判读。最近深入沙漠腹地的实地考察引发了对该沙漠"羽毛状"沙丘的争论。本文从地质构造、遥感影像纹理特征、沙丘形态特征、风况特征、组成沙丘沉积物的粒度特征、矿物组成、光谱特征、颗粒形貌等多层次、多视角探讨库姆塔格沙漠的"羽毛状"风沙地貌。提出从三种空间尺度上区分"羽翼状"沙漠、"羽毛状"图案(伪羽毛状沙丘)和"羽毛状"沙丘的必要性。认为:①库姆塔格沙漠的"羽翼状"总体格局是受新构造运动控制的。②以往基于航片判读确认的"羽毛状"沙丘实际上是由线性(赛夫)沙丘、丘间走廊的亮色浮沙片和残余暗色粗沙地的反照率对比形成的"羽毛状"图案,并非真正的复合沙丘。③真正的"羽毛状"沙丘应该是指有明显新月形沙丘遗留翼角的赛夫沙丘(线性沙丘)的变型。④由赛夫沙丘到"羽毛状"沙丘,风况愈来愈复杂。 展开更多
关键词 风沙地貌 羽毛扇”状沙漠 “羽毛状”图案 “羽毛状沙丘
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A Study of Kumtag Desert:Progresses and Achievements 被引量:1
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作者 王锋 褚建民 +4 位作者 王学全 崔向慧 吴波 杨文斌 卢琦 《Journal of Resources and Ecology》 CSCD 2011年第3期193-201,共9页
The Kumtag Desert, the fourth largest sand desert covered mainly by mobile dunes and shifting sands, had remained as the last untouched natural desert to be fully investigated in a scientific way. Therefore,"Integrat... The Kumtag Desert, the fourth largest sand desert covered mainly by mobile dunes and shifting sands, had remained as the last untouched natural desert to be fully investigated in a scientific way. Therefore,"Integrated Scientific Expedition of the Kumtag Desert Programme"was listed as one of nine key research programmes of China National Science and Technology Basic Research Programmes in December, 2006. The expedition team carried out two large-scale and multidisciplinary scientific expeditions from June 2007 to December 2009, to the Kumtag Desert and collected more than 20 sets of field samples and ground observations. Finally, the expedition team completed not only systematic and integrated scientific expedition of the Kumtag Desert and filled in the gap of the last unexplored desert in China, but also gained fruitful research results in many scientific research subjects. These research results included that:(i) A unique aeolian landform unit, sand-gravel-moraine, developed in the Kumtag Desert, was defined and named for the first time, and the morphologic characteristics of feather-like longitudinal sand dune and its formation process are initially proved;(ii) Two sources and mineral element composition of the surface sedimentation of the Kumtag Desert was determined, and the characteristics of the desert sedimentation and stratum chronology of the Later Cenozoic Era was illustrated;(iii) The chronology of the paleo-aeolian sand was essentially determined and the formation courses and evolution process of the desert was illustrated;(iv) The thorough investigations of water system distribution, hydrology,chemical characteristics of water of the Kumtag Desert were made and six Water System Evolution Maps of the Kumtag Desert were compiled from the Later Cenozoic Era to the contemporary age;(v) The types, formation processes and distribution of soil in the Kumtag Desert were fully determined;(vi)An all-direction, all-weather, full-coverage desert meteorology observation was established and the characteristics and trend of climate change of the Kumtag Desert and nearby districts were adequately illustrated;(vii) It is the first time that the distribution areas of six plant species, including Tamarix taklamakanensis, Tamarix albiflonum, Agriophyllum lateriflorum etc., were catalogued in the Desert;(viii) The varieties, population, quantity and distribution of the wild animal such as the Bactrian Camel (Camelus ferus Przewalski), are now documented;And (ix) it is the first time that the ecological services and economic function subdivision zones of the Kumtag Desert were classified;the Framework of the Great Dunhuang Special Ecological-Economic Zone was proposed to realize the sustainable development strategy in population, resources, environment, ecology and economics in the Kumtag Desert and nearby districts. 展开更多
关键词 scientific expedition Kumtag Desert feather-like longitudinal dunes sand-gravel-moraine Bactrian Camel Dunhuang
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