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英語(yǔ)人>詞典>漢英 : 干冷的 的英文翻譯,例句
干冷的 的英文翻譯精品中文字幕一区二区三区四区、例句

干冷的

基本解釋 (translations)
crispest

更多網(wǎng)絡(luò)例句與干冷的相關(guān)的網(wǎng)絡(luò)例句 [注:此內(nèi)容來(lái)源于網(wǎng)絡(luò)欧美日韩在线一区二区,僅供參考]

According to reports, the winter cold, dry weather is apt to cause exfoliative cheilitis, tongue licking cheilitis cheilitis, and simple.

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Low degree-day factors can be expected for cold-dry areas, whereas, high degree-day factors can be expected for warm-wet areas in western China.

總體看來(lái)日韩无码一级黄色毛片,西部冰川的度日因子由西北向東南逐漸增大久久园产黄色大片视频,這與中國(guó)西部冰川的氣候環(huán)境變化趨勢(shì)是一致的99视频精品免费99在线,即在干冷的氣候條件下,度日因子較泄?00部自拍视频在线播放w。av;而在暖濕的氣候條件下度日因子較大。

The study has shown:(1) With increasing sediment depth and the woody giblets, the total organic carbon, the extraction of benzene , the total humic acids and the unhydrolyte are enhanced, while the hydrolyte is decreasing.(2) According to the GC-MS analysis, n-alkane,n-alkan-2-ones and n-alkanones are composed mainly of long-chains,such a result is thought to be characteristic of a herbaceous input from 2300a.B.P. n-alkanones exist in the samples may be considered as the evidence of microorganisms activity.(3) It is showed that the lipids is more sensitive to the climate change than the floristic. The proxy of the pollen spore of the peat stratum is different from the normal environment proxy. It is one of the main reasons that the sensitivity difference of the bog vegetation reacting to the climate isn't accordant with the log of the fat molecule fossil and biology fossil.(4) The transformation of the peat organic carbon is under the influence of temperature,acidity,organic material constituting, etc, and it showed the up-trend with the depth. In the short-term scale, the conversion of the peat organic carbon is effected by seasonal water,regional climate and vegetations; while in the long-term scale, it is controlled mainly by the climate.(5) According to the comparing the orderliness of organic compound,vegetation giblets with the depth to the characteristics of the peat molecule fossil with the section, in the development of this peatmire, 1500a B.P(210cm)is regard as the borderline of the late Holocene, the keynote of the front period is warm with several cold fluctuations, and the trend of the back period is dry and cold although there were several fluctuations.

研究表明:(1)隨深度的增高及植物殘?bào)w中木本殘?bào)w的增多91囯内自拍,總有機(jī)碳亚洲欧美国产国产综合二页、苯萃取物、總腐植酸久久精品免费精品、不被水解物含量逐漸增高一级a性色生活片厕所偷拍,而易水解物含量減少;(2)GC- MS分析顯示女人被做到高潮连连免费视频,正構(gòu)烷烴線上A片,直鏈烷基2-酮和正烷醇均以長(zhǎng)鏈組分為主,揭示了該泥炭柱剖面2347a.B.P的母源輸入以草本植物為主欧美性日;甲基酮類和短鏈正烷醇的存在是微生物活性很大的生物證據(jù)欧美性爱在线播放网站;(3)通過(guò)有機(jī)分子標(biāo)志物與孢粉、植物殘?bào)w等指標(biāo)的對(duì)比研究表明:脂類化合物對(duì)氣候變化的反映要比植物種靈敏得多午夜福利97,不同沼澤植物對(duì)氣候變化的敏感性的差異是脂類分子化石記錄與生物大化石結(jié)果很難一致的主要原因之一日韩在线精品福利网页视频观看免费;(4)泥炭有機(jī)碳的轉(zhuǎn)化受到溫度、酸度一级特黄AAA免费看直播、有機(jī)物質(zhì)組成等很多因素的影響免费观看无码视频,短時(shí)間尺度,泥炭有機(jī)碳的轉(zhuǎn)化受季節(jié)性降水国产亚洲精品麻豆一二三区、地方氣候和植被等因素的影響亚洲日本黄色视频;長(zhǎng)時(shí)間尺度,泥炭地有機(jī)碳的轉(zhuǎn)化有色永久无码视频在线观看,受氣候條件控制中文字幕无码一区在线视频青青;(5)總結(jié)泥炭分子化石特征、泥炭有機(jī)質(zhì)各組分含量及植物殘?bào)w組成隨深度的變異規(guī)律免费无码十八禁污污网站,分析結(jié)果顯示該泥炭地層形成過(guò)程中欧美人做一级视频,1500a B.P(210cm)可作為劃分前后晚全新世的界線,前期的基調(diào)是氣候偏暖午夜成年男人免费网,但又有幾次偏干冷氣候的反復(fù)无码AAA片毛片观看,后期氣候以干冷為主,其間雖有幾次上升波動(dòng)一级AAAAA大黄片,但整體趨勢(shì)不變无码黄片在线看。

Of vitamin D. people in cold dry climates became stocky, to conserve heat.

在干冷氣候里生活的人變得低矮結(jié)實(shí),可以保持熱量黄片久久久动漫。

Combined with research of archaeological time and civilization stages, the physical environment change of Wuhan district during middle and late Neolithic Age is reconstructed in detail, which comes through stages of warm and humid, semi\|warm and semi\|humid, dry and cold, relatively torridity and humid, warm and humid successively.

運(yùn)用植硅石分析新方法對(duì)武漢周邊先秦遺址考古土壤進(jìn)行分析研究jiizz日本护士老师高潮,發(fā)現(xiàn)其中植硅石含量豐富97大学生情侣酒店自拍亚洲精品,且具有一定的組合分帶性,結(jié)合考古年代與文化期研究免费在线看黄色国产,揭示出武漢地區(qū)新石器中晚期( 50 0 0 - 2 70 0 a BP)氣候環(huán)境變化信息国产麻豆区精品系列在线,即先后經(jīng)歷了溫濕期、溫涼期日韩偷窥无码少妇AV、干冷期亚洲狠狠草视频、暖濕期、溫濕期国产精品自拍观看。

Keeps his skin moisturized and soft especially during the cold dry weather.

使得他的皮膚柔軟久久av免费不卡天堂小草播放、滋潤(rùn)激情一级a片在线播放,特別是在干冷的冬天黄色视频在线观看品。

During the last 1 Ma,Zhongtan underwent nine moist hot-dry cold cycles,three winter monsoon intensifications,and three extremely dry events.

在過(guò)去1 Ma以來(lái),中灘黃土及河漫灘剖面的地層特征被强制伦A片在线观看、粒度曲線表明其記錄了9個(gè)濕熱干冷氣候旋回日韩一级大日韩女大片一级,3次冬季風(fēng)強(qiáng)化階段,存在著3次極端干旱事件人人干,人人草。

A few days ago, in the class is on the way, cold, dry air gave me cold Such is Life, she felt as a stiff ice, suddenly, the sky it began to snow in just a few minutes, the glass was decorated numerous flowers.

前些天欧欧美一级a爱高清成在线看,在下課的路上,干冷的空氣讓我寒冷入骨欧美一级黄片久久久久久久,感覺(jué)自己像一塊僵冰欧美一区二区三A片,忽然,天空下起了小雪久久久久久A级片,短短幾分鐘国产高清无码强奸视频网址,玻璃被無(wú)數(shù)花朵點(diǎn)綴。

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.

地層沉積相及粒度黄色性爱欧美狂野澳门、磁化率插插受不了视频、化學(xué)元素、孢粉和古脊椎動(dòng)物化石等氣候代用指標(biāo)的測(cè)試分析人人操人人射人人干,揭示了研究區(qū)末次間冰期以來(lái)氣候有過(guò)多次干冷国产800AV私人在线观看、暖濕波動(dòng),曾經(jīng)歷了干冷的干旱荒漠国语对白露脸刺激自拍、干旱荒漠草原潮喷人人操、半干旱干草原、溫濕灌叢草原或疏林草原三级片黄片日韩、溫暖半濕潤(rùn)森林草原氣候環(huán)境的交替變化视色视频免费在线观看。

A second dish of fresh, home-made tagliatelle pasta was tossed with vine-ripened cherry tomatoes and homemade ricotta.

壓碎的橄欖和一杯干冷的Catalan白酒先上桌,橄欖多而且多汁來(lái)黄色网站日韩观看免费,自比Catalan海岸更遠(yuǎn)的地方肏丝袜屄影片,酒杯在我手里結(jié)水珠日韩mv在线看成人网站。

更多網(wǎng)絡(luò)解釋與干冷的相關(guān)的網(wǎng)絡(luò)解釋 [注:此內(nèi)容來(lái)源于網(wǎng)絡(luò),僅供參考]

Philosophy:自然哲理

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and drizzling:觸不到溫暖

看不見(jiàn)藍(lán)天 dry cold | 觸不到溫暖 and drizzling | 干冷的 cannot feel the warm

bise:比士風(fēng)地中海北岸一帶干冷的北風(fēng)

biscuit 床墊餅干 | bise 比士風(fēng)地中海北岸一帶干冷的北風(fēng) | bise 地中海北岸一帶干冷的北風(fēng)

bise:地中海北岸一帶干冷的北風(fēng)

bise 比士風(fēng)地中海北岸一帶干冷的北風(fēng) | bise 地中海北岸一帶干冷的北風(fēng) | bisect 二等分