祁连山南坡,southern slope of Qilian Mountain
1)southern slope of Qilian Mountain祁连山南坡
1.Vegetation landscape pattern and its fragmentation onsouthern slope of Qilian Mountain.祁连山南坡植被景观格局及其破碎化
英文短句/例句
1.Vegetation landscape pattern and its fragmentation on southern slope of Qilian Mountain.祁连山南坡植被景观格局及其破碎化
2.The Features of Microclimate and Vegetation Distribution on the Southern Lenglonglin,Qilian Mountains祁连山冷龙岭南坡小气候及植被分布特征
3.An Afforestation Experiment on the Arid Area of North Hillside in East Part of Mountain Qilian祁连山东段北坡干旱浅山区造林试验
4.Northwest-to-Southeast Mountain Ranges, including the altay, Qilian and Gangdise Ranges;西北-东南走向:阿尔泰山、祁连山、冈底斯山等。
5.Study on Moss Distribution Law in Different Altitude on North Slope of Qilian Mountains祁连山北坡不同海拔梯度苔藓分布规律研究
6.Research on Community and Species Diversity of Picea Crassifolia Kon Forests in the North Slope of Qilian Mountain;祁连山（北坡）青海云杉群落物种多样性研究
7.Study on the Zone of Maximum Precipitation in the North Slopes of the Central Qilian Mountains祁连山中段北坡最大降水高度带观测与研究
8.According to the survey, the vertical distribution character of vegetation on the north slope of the east part of Qilian Mountains was studied.根据调查，对祁连山东部北坡的植被垂直分布特征进行了分析研究。
9.Analysis on the Distribution Pattern of Grass-Picea crassifolia Forest Dominant Population in the Northern Slope of Qilian Mountains祁连山北坡草类—青海云杉林优势种群分布格局分析
10.Vertical distribution and diversity of butterflies in the northern slopes of Qilian Mountains and Hexi Corridor祁连山北坡及河西走廊蝶类垂直分布及群落多样性研究
11.The elevational patterns of β diversity of Picea crassifolia communities on northern slope of Qilianshan Mountain祁连山北坡青海云杉群落β多样性垂直分布格局
12.Precise Timing and Significance of Caledonian Structural Deformation Chronology in Southeast Qilian祁连山东南段加里东造山期构造变形年代的精确限定及其意义
13.The traits of α and β diversity of different habitats of alpine grassland plant community in Eastern Qilian Mountains were studied.对东祁连山高寒草地不同生境类型（阴坡、滩地和阳坡）植物群落的α和β多样性进行了研究。
14.THE ZHOULANGNANSHAN CALEDONIAN SUBDUCTIVE COMPLEX IN THE NORTHERN QILIAN MOUNTAINS AND ITS DYNAMICS北祁连走廊南山加里东俯冲杂岩增生地体及其动力学
15.They also do not belong to the south meta-volcanic rock series of Northern Qilian Caledonides tectonic belts.也不属于北祁连加里东构造带南带变质火山岩系的一部分。
16.DISCOVERY AND AGE-SIGNIFICANCE OF SPONGE FOSSILS OF KESUER FORMATION IN THE SOUTHERN MARGIN OF EASTERN MIDDLE-QILIAN MOUNTAIN中祁连山东段南缘克素尔组海绵类化石的发现与时代讨论
17.ANALYSIS ON THE ECONOMIC BEHAVIOR OF THE HERDSMAN IN THE HEXI CORRIDOR--A Case Study of Sunan County;河西走廊祁连山区牧户经济行为分析——以肃南县为例
18.Soil Organic Matter and Total Nitrogen Changing with Altitudes on the Southern Foot of Eastern Qilian Mountains祁连山东段南麓不同海拔土壤有机质及全氮的分布状况
相关短句/例句
Southern foot of East Qilian Mountains祁连山坡地
3)northern of Qilian mountains祁连山北坡
1.The text opening out the continuance climate warming is the essence characteristic ofnorthern of Qilian mountains.本文揭示了气候持续变暖是祁连山北坡现代气候变化的基本特征。
4)northern slope of Qilian Mountains祁连山北坡
1.Investigating the rodent population onnorthern slope of Qilian Mountains, 2 order 6 family 14 genus 23 species of rodent animals were found and the diversity of rodent animal population reduced with rising of elevation.对祁连山北坡啮齿动物种群调查,共发现啮齿动物2目6科14属23种,啮齿动物种群多样性随海拔的升高而降低,并提出了该地的主要鼠害种类及控制建议。
5)southern foot of Qilian mountains祁连山南麓
1.The litter water-holding capability of the artificial plant communities of the rehabilitated land in Datong county of Qinghai province located at thesouthern foot of Qilian mountains was studied.对位于祁连山南麓的青海省大通县退耕地人工植物群落的枯落物容水性能进行了研究。
6)Danghe Nanshan in the Qilian Mountains祁连山党河南山
延伸阅读
祁连山祁连山Qilian ShanQiliQn Shan祁连山(Qilian shan)中国青藏高原东北边缘山脉。匈奴语呼天为“祁连”，故名。位于青海、甘肃两省交界处。西起当金山口与阿尔金山山刀永相接，东至黄河谷地与秦岭、六盘山相连，南抱柴达木、共和盆地，北临河西走廊。亦称走廊南山。东西长达1 000千米，南北宽200一300千米，面积20.6万平方千米。由一系列西北一东南走向的平行山脉和山间谷地组成。地势西北高、东南低，北坡陡峻，南坡和缓。山峰海拔多在4 000米以上，最高峰为疏勒南山团结峰(又名宰吾结勒)，海拔5 808米。山体多由石灰岩、花岗岩组成。海拔4 500米以上的山峰终年积雪，冰川广布。祁连山由西向东分为三段。西段为疏勒河上游谷地以西。自北至南有照壁山、大雪山(野马山)、野马南山、党河南山、察汗鄂博图岭、土尔根达板和柴达木l一日。山势高峻，海拔多在3 500~5 000米之间，主峰大雪山海拔5 483米。大部山坡植被稀疏，阴坡生长小片针叶林及灌木林。发源西段的疏勒河、党河，流人河西走廊。位于阿尔金山脉和祁连{妇交接处的当金山口是重要隘口，海拔3 649米，南北长约27千米，谷狭路隘，两侧山峦重迭，奇峰陡立，地势险要。柳园一格尔木公路从山口通过，是沟通河西走廊和柴达木盆地间的重要通道。距嘉峪关市81千米的镜铁山铁矿一，储量大，全国闻名。中段为疏勒河上游谷地至扁都口。由北向南有走廊南山、托来山、托来南山、疏勒南山、哈拉南山、宗务隆山、青海南山，其间夹有黑河谷地、青海湖盆地。主峰祁连山海拔5 547米。阴坡峡谷，林木茂密，生长云杉林及冷杉林，海拔4 000米以上植被稀少。北麓水源丰富。共有大小河流12条，其中黑河最大。南麓干燥，植被稀少。由西北向东南有近28个沟口，北距甘肃省民乐县28千米处的扁都口最为重要，是西宁一张掖公路之咽喉。扁都沟贯通南北，沟长32千米，谷宽仅30一200米，海拔3 200-4 150米。两侧山峰连绵起伏，多为悬崖绝壁，山坡灌木丛生，童子坝河沿沟北流。山间溪多流长，水质良好。有西宁一嘉峪关的公路经扁都口斜穿山地，是青海和一甘肃间又一通道。东段为扁都口以东。自北向南有冷龙岭、乌稍岭、大通山、拉脊山等，海拔2 400一3 500米。冷龙岭最高，海拔4 843米。海拔3 000米的阴坡、谷底，为茂密的森林和草原;3 200一4 000米为高山草原草甸及灌木林。阳坡均为山地草原。大通河由西向东流，河谷地势低平。盐矿资源丰富。青海湖为中国最大咸水湖泊，周围为良好草场，是发展畜牧业的理想地区。煤矿储量丰富，著名的有木里一江仓煤矿和九条岭煤矿。有兰州一乌鲁木齐铁路、公路南北纵穿。西段为高寒大!淤哇干旱区，中段和东段为高寒大陆性半干旱区，1月平均气温一16-一10℃，7月平均气温9一16℃。东段夏季雨水较多，中段为湿润干燥过渡区，雨量渐少，西段极端干燥。最大冻土深1.5一2.0米。祁连山山体庞大，山势险峻，为河西走廊的重要依托。(张立学)祁连山一瞥孟昭瑞摄
