草原

基本解释 (translations)

campo  ·  grassland  ·  lea  ·  plain  ·  veldt  ·  campos  ·  grasslands  ·  veld

与草原相关的网络例句 [注：此内容来源于网络，仅供参考]

White clouds wave in the blue sky, horses run below the white clouds, this is our Chinese people's sung and impressions on the grasslands, but in my feelings, grassland and the world is a unity, in the vast grassland the pure clean river is the most breeziness and dazzling , she's like a white cincture of Earth, also like a white hada, flying in the green sea, flying in melodious melody of Matou Qin, cattle and sheep and tabernacle is like a piece of cloud , the spray, the note are telling the story of the prairie.

作品描述：蓝蓝的天上白云飘，白云下面马儿跑，这是中国人对草原的传唱和印象，而在我的感受里，草原的天地和人是合一的，在茫茫的草原里最灵动、最耀眼的是那条纯净的清流，她像一条地球的白飘带，又像一条洁白的哈达，飘舞在绿色的海洋里，在马头琴悠扬的旋律中飞翔。牛羊和帐房仿佛是一片片云彩，一朵朵浪花，一个个音符在诉说着草原的故事。

The Farming-pastoral Zone in North China was separated into 8 Eco-regions according to the known Eco-region. The dissertation analyzed the regional differences of land use changes from three aspects on dynamic degree , land use degree and the change direction (1)On land use dynamic degree, the dynamic degree of the cropland was the highest in North warm temperate deciduous broad-leaved forest and the lowest in temperate forest steppe; forest land's was the highest in alpine meadow and the lowest in warm temperate forest steppe; grassland's was the highest in temperate forest steppe-bunchgrass steppe and the lowest in alpine meadow; other land's was the highest in North warm temperate deciduous broad-leaved forest－the Huang-Huai-hai plain and the lowest in warm temperate bunchgrass steppe.

结合已有的自然生态区的划分，将我国北方农牧交错带划分为8 个自然生态区，选取土地利用动态度、土地利用程度以及土地利用变化方向等3 个方面的指标对研究区进行了区域分异规律的研究，结果如下：（1）耕地动态度北暖温带落叶阔叶林生态区——北部山地丘陵区最大，温带森林草原生态区最小；林地的动态度高寒草甸生态区最大，暖温带森林草原丛生禾草草原生态区——东南森林草原区最小；草地动态度温带森林草原——丛生禾草草原生态区最大，高寒草甸生态区最小；其他用地的动态度北暖温带落叶阔叶林生态区——黄淮海平原区最大，暖温带森林草原丛生禾草草原生态区—西北丛生禾草草原区最小。

This also let me make to understand why the horde of steppe's canning live on the steppe still can chase steppe conservancy for several thousand years so complete, but agriculture race once stepping into the steppe didn't lead for several years, the steppe disappears, leaves an one slice a hungriness.

这也让我弄懂了为什么草原上的游牧民族能够在草原上生活数千年却依然能够把草原保存的那么完整，而农耕民族一旦踏入草原，没过几年草原就消失了，只留下一片片荒漠。

In the days when everybody started fair, Best Beloved, the Leopard lived in a place called the High Veldt.

亲爱的孩子们，在所有的动物颜色都一样的日子里，豹子生活在一个叫高地草原的地方，记得那不是低地草原，也不是未开垦的草原，更不是酸味十足的草原，而是绝对裸露、炎热、阳光充足的高地草原。

In terms of 家在草原's case, the issue at stake is not politics, but basic human rights and dignity - no one denies that Tibet is occupied at the moment.

在的学期家在草原's事，出版危如累卵是不政治，但是基本人正义和尊严-没有人兽穴那西藏是占此刻。

Four typical grassland communities, Stipa klemenzii, Stipa grandis, Leymus chinensis and Leymus chinensis + forbs, had been chosen along precipitation gradients from 200, 290, 350 to 450 mm respectively in Inner Mongolia Steppe. The objectives of this study were to determine the effects of grazing on plant community composition, aboveground and belowground biomass, species and functional group diversities and the relationship between diversity and productivity, the effects of grazing on soil seed bank species composition, seed density and diversity along the transect.

选取内蒙古草原三种主要草原类型(草甸草原、典型草原和荒漠草原)代表性群落羊草杂类草群落、羊草群落和大针茅群落、小针茅群落，应用样线法沿水分梯度研究放牧对内蒙古草原不同植物群落功能群组成、多样性、生产力以及多样性与生产力关系的影响和放牧对土壤种子库组成、大小以及多样性的影响，在此基础上，研究土壤种子库与地上植被间的关系。

From 6860 to 3170 cal.yr BP,semi-desert steppeexpanded,regional montane forest steppe retreated,suggesting a prolonged warm and dryclimate.Between 3170 and 2340 cal.yr BP,regional forest steppe expanded whereassemi-desert steppe retreated,indicating the climate became cool and wet gradually and thehumidity reached the maximum at the end of this stage.During 2340～1600 cal.yr BP,Poaceae steppe dominated whereas wetland meadow expanded and the montane forest stepperetreated,suggesting a cool and wet climate prevailed,wormwood grass steppe prevailed andthe climatic instability increased after 1600 cal.a BEThe climate and environmental reconstructions by pollen were supported by the diatomrecords.A relative high lake level and moister climate prevailed between 8660 and 7230 cal.yr BP as inferred by the dominance of planktonic diatom genera and high planktonic/benthicratio (〉40).low lake level and dry climate sustained during 7230～2330 cal.yr BP assuggested by the low abundance of planktonic diatom and low planktonic/benthic ratio ～20and the lake returned to high level during 2330～930 cal.yr BP as inferred by there-dominance of the planktonic diatom and the high value of palnktonic/benthic ratio.The pollen-based climate reconstruction was also consolidated by the grain size andPediastrum concentration records.

Ugii Nuur湖周围现代孢粉研究表明：松属为空气传播的外来花粉，其含量变化可能指示了远山森林草原发育状况；禾本科具显著低代表性，母体植物建群时含量通常在10％以下：藜科花粉含量可以指示区域气候干旱程度。2、以现代孢粉研究为基础、可靠AMS~(14)C年代为框架，Ugii Nuur孢粉记录高分辨率地重建了蒙古国中部地区过去8660 cal.yr BP以来的植被和气候变化。8660～7800 cal.yr BP研究区植被为禾草草原，湖畔及河谷低地发育苔草草甸，远山发育松属针叶林和森林草原，气候温和略湿润；其中8350～8250 cal.yr BP湿生草甸扩张，旱生植物成分减少，气候凉湿。7800～6860 cal.yr BP旱生成分增加，气候转向暖干。6860～3170 cal.yrBP半荒漠草原扩张，远山森林草原退缩，山地草原和河谷及湖畔湿生草甸退缩，气候持续暖干。3170～2340 cal.yr BP半荒漠草原退缩，远山森林草原扩张，气候转凉变湿，末期湿度条件达最佳。2340～1600 cal.yr BP禾草草原发育，湖畔及河谷低地湿生草甸扩张，远山森林草原略有退缩，气候总体较凉湿。1600 cal.yr BP以来研究区发育禾草-冷蒿草原，气候波动较大。

It also suggested that the climate and environment in the area are characterized by changeability, sensitivity, instability, its general changes are the positive process of desertification correspondingly to the dry-cold steppe or desert steppe and desert, while the reverse process correspondingly to warm semi-humid forest steppe and temperate-humid shrub steppe.

进一步证实了古土壤S〓发育和河湖相沉积的萨拉乌苏组堆积时为温暖半湿润的森林或森林草原环境，全新世的砂质古土壤或湖沼相沉积时为温湿灌丛草原或疏林草原环境，黄土沉积时为半干旱干草原环境，风成砂沉积时为干旱荒漠草原甚至荒漠环境。

Analysis of sedimentary facies and the multiple proxy indexes indicate that climate have many times dry-cold and warm-wet changes in the desert-loess transition belt since the last interglacial, and environment undergone alternations from warm semi-humid forest steppe, temperate-humid shrub steppe, semi-arid steppe and dry-cold steppe, desert steppe to desert.

地层沉积相及粒度、磁化率、化学元素、孢粉和古脊椎动物化石等气候代用指标的测试分析，揭示了研究区末次间冰期以来气候有过多次干冷、暖湿波动，曾经历了干冷的干旱荒漠、干旱荒漠草原、半干旱干草原、温湿灌丛草原或疏林草原、温暖半湿润森林草原气候环境的交替变化。

P in Shule River Alluvial Fan Oasis in Gansu subsidized by CNSF. Through field geological and environmental observations and sampling, quartz OSL dating, organic carbon ~(14)C dating, as well as analysis of TOC,grain size and Pollen assemblage of the samples from ten sediment profiles in front fine grain sediment zone of the Shule River Fan, the results obtained as follows:(1)The vegetation evolution history on Shule River Alluvial Fan and circumjacent since about 13 ka B.P. could be divided into 6 phases: about 12.1-13.1ka, a sparse coniferous and broadleaf trees - shrub grassland, cold and wet climate; 9.2-12.1ka, shrub grassland, temperature rising but precipitation and humidity getting down; 5.8-9.2ka, sparse forest with the most flourish shrub grassland under the optimal climate; 4.3-5.8ka, coniferous and broadleaf mixed forests -shrub grassland, temperature rising slightly and getting dry; 4.3-2.8ka, grass vegetation and climate became more dry; 2.8-2.3ka, coniferous forests -shrub grassland, precipitation and temperature getting down, but a higher relative humidity.

本文依托于&甘肃疏勒河冲积扇5万年来古天气环境与古水文演化&项目，以疏勒河冲积扇为研究对象，通过对疏勒河冲积扇扇缘细土带全新世古天气和古水文演变进行了20余个剖面的观测和取样、石英OSL和~(14)C测年、粒度组成和TOC分析以及孢粉鉴定，获得了以下成果和熟悉：(1)距今约13ka年来冲积扇和周边植被演化经历了6个阶段：约13.1～12.1ka，以针叶林为主的针阔混交林～灌丛草原，天气冷湿；12.1～9.2ka，灌丛草原，气温升高，降水量较低；9.2～5.8ka，疏林灌木草原，植被茂盛，温度和降水最佳；5.8～4.3ka，以针叶树为主的针阔混交林～灌丛草原，气温较高，降水减少；4.3～2.8ka，草原植被，天气变干；2.8～2.3ka，针叶林～灌木草原，降水减少，温度降低，相对湿度有所增加。

与草原相关的网络解释 [注：此内容来源于网络，仅供参考]

Campo：巴西草原 旱性草原(巴西的)

campestral 田间的,田野的,先于田野的,野栖的 野棲的 Y | campo 巴西草原 旱性草原(巴西的) Y | campo cerrado 巴西疏林草原 疏林草原(巴西的) Y

campo sujo：巴西稀树草原 疏木草原(巴西的)

campo cerrado 巴西疏林草原 疏林草原(巴西的) Y | campo sujo 巴西稀树草原 疏木草原(巴西的) Y | cane 细长的茎,藤条 木質性禾木; 實心杆; 結果母枝 Y

campo cerrado：巴西疏林草原 疏林草原(巴西的)

campo 巴西草原 旱性草原(巴西的) Y | campo cerrado 巴西疏林草原 疏林草原(巴西的) Y | campo sujo 巴西稀树草原 疏木草原(巴西的) Y

prairie：北美草原

温带草原是陆地主要生态系统之-,分布于内陆干旱到半湿润气候区,主要有欧亚大陆草原(steppe)、北美草原(Prairie)和南美草原(Pampas)等. 草原区具大陆性气候,四季分明,夏季温暖,冬季严寒、年均降水量约250~500 mm,多集中夏季,

Marginal rangeland：边际草原, 边缘草原

Marginal range 边际草原, 边缘草原 | Marginal rangeland 边际草原, 边缘草原 | Maine prairie 海洋普列里, 海洋草原

savanna climate：热稀稀树(干)草原气候

savanna 热带稀树(干)草原;疏林草原 | savanna climate 热稀稀树(干)草原气候 | savanna woodland 热带稀树(干)草原林地

steppe：典型草原

第二章至第七章为原则篇或基础篇,以草地...鄂尔多斯草原(ORDOS GRASSLND)从植被地理学和植被生态学来划分,它包含着:典型草原(Steppe)、荒漠草原(Desert Steppe)和草原化荒漠(Steppe Desert)三种草原类型,是覆盖鄂尔多斯高原地带性植被的总...

forest steppe：森林草原

森林草原(Forest Steppe)是温带落叶阔叶林与草原之间的过渡带,也就是这两个地带间的群落交错区(或称生态过渡带). 它是一种较均匀的植被类型,而是落叶林和草甸草原的大型镶嵌体. 在这个过渡带上,最初落叶林占优势,草原呈分散的岛屿,

steppe soil：草原土,草原土壤

steppe plant 草原植物 | steppe soil 草原土,草原土壤 | steppe type of soil formation 草原成土作用

Campine：刚果稀树草原, 非洲稀树草原

California steppe 加利福利亚草原 | Campine 刚果稀树草原, 非洲稀树草原 | Campo limpo 巴西无树高草地