月壤 的英文怎麼說

中文拼音 [yuèrǎng]
月壤 英文
chip
  • : Ⅰ名詞1 (月球; 月亮) the moon 2 (計時的單位) month 3 (姓氏) a surname Ⅱ形容詞1 (每月的) mo...
  • : 名詞1. (土壤) soil 2. (地) earth 3. (地區) area 4. (姓氏) a surname
  1. Through analyzing guan zi, zhao guo, fan sheng zhi shu, si min yue ling and other agricultural books, some agronomists on agricultural education, it states that in west han and east han dynasties agricultural science and technology made great progress, such as soil and tillage, drainage and irrigation, farm implements, crop cultivation, gardening, silkworm raising and mulberry growing, environment and ecology, agricultural economics and management

    通過對《管子》 、趙過、 《 ?勝之書》 、 《四民令》等農書及農業科學家農業教育的闡述,指出了兩漢時期的農業教育主要在農業科技教育方面取得進展,具體體現在土耕作教育、農田水利教育、農機具教育、作物栽培知識教育、園藝知識教育、蠶桑知識教育、環境生態教育、農業經濟管理教育等方面。
  2. Seven plots selected from wanglang reserve were distributed in different types of forest and at different altitude, and different plot has different microclimate. soil property, microbial population, soil nutrient content of forest soil were determined in wanglang natural reserve, from may to october 2002 to july 2003, the ecological distribution of three main groups, bacteria, actinomycete and fungi were determined in the forest soils by the cell enumeration methods. six kinds of physiological groups, including ammoniation bacteria, nitrification bacteria, nitrosification bacteria, aerobic autogenesis azotobacter, aerobic cellulose - decomposing bacteria and anaerobic cellulose - decomposing bacteria were enumerated by the most - probable number ( mpn )

    2001年10在王朗自然保護區內設立了3個定位研究樣地和4個臨時樣地,通過多次現場采樣與室內實驗分析,測定了白樺林、岷江冷杉林、紫果雲杉林、繡線菊-羊茅群落、羊茅群落及高山柳灌木叢等6種不同植物群落內土微生物三大類群數量、功能微生物數量、土養分,並在固定樣地內使用埋袋法進行了三個埋藏深度的凋落物分解袋試驗,初步研究了枝條、闊葉、針葉等凋落物組分在不同分解階段所含養分的動態變化。
  3. It can germinate at 0 ? and develop at 3 - 5 c even suffer from chilliness of - 21 c. at the fifth or sixth year, it ablooms at july, fruits at august or september. when the seeds are scattered by wind, the plant turn to death

    其自然生長環境的土偏酸性,有機質含量極低,氣候多變,最高平均溫度3 5 ,最低平均溫- 19 - 21 ,年降水量800mm ,無霜期僅有50d左右。
  4. Specific diversity of soil amoebae and flagellates in the national nature reserve of baishuijiang, gansu was studied based on the " non - flooded petri dish method " and the observation in vivo from february 2004 to may 2006

    摘要2004年22006年5,用「非淹沒培養皿法」和活體觀察法對甘肅白水江國家級自然保護區土肉鞭蟲的物種多樣性進行了研究。
  5. C. test samples included ilmenite and minnesota lunar simulant, or mls - 1a

    實驗的樣本包括鈦鐵礦和明尼蘇達模擬球土mls - la 。
  6. 3. it is exert through cultivated in a pot experiment cultivation for two month lindane and ddt original pesticide experiment after two month to get soil examine appearing value very low to find to observe. soil sampled form j and n farm which have used lindane and ddt for 40 years, the analysis result showed that the residue of the two pesticides are very high. lindane remains and reaches as high as 996. 06 g kg - 1, and ddt is 3382. 75 g kg - 1 4

    經過盆栽實驗兩個的培養觀察發現施加到土中的林丹與ddt原藥在兩個的實驗后檢出值較低具有使用林丹、 ddt四十年歷史的北京近郊j 、 n農場中兩種農藥殘留較高,林丹殘留最高可達: 996 . 06 g ? kg ~ ( - 1 ) , ddt殘留最高可達: 3382 . 75 g ? kg ~ ( - 1 ) 。
  7. How to choose between them ? arenas was shaky in november before this otherworldly december ; caron butler has been washington ' s most consistent player

    如何從他們之間選擇?阿里納斯11的不穩定的表現和他在12的表現成天之別;卡龍巴特勒成為華盛頓最穩定的球員。
  8. Effects of soil water content level on net photosynthetic rate and chlorophyll fluorescence parameters in pistachio leaves

    含水量對阿渾子葉片凈光合速率及葉綠素熒光參數的影響
  9. Putting forward to the clear and definite concept and principia in proseminar ", the sustained land management evaluation in developing country ", and " the sustained land management ( using ) hi 21st century " point out : the land using is to combine the technique, policy with the social economic principle and the incorporated behavior of circumstance relation, in order to attain the keeping or increasing production or services at the same time, lowering the production risk, keeping nature resources potential and preventing the soil degeneration, making its have the economic vitality and accepted by the social

    土地資源的可持續利用是可持續發展的基礎,沒有土地資源的可持續利用就不可能有可持續發展。 1991年9在泰國清邁舉行的「發展中國家持續土地管理評價」研討會和1993年6在加拿大舉行的「 21世紀持續土地管理(利用) 」國際會議上提出了持續土地利用的明確概念和基本原則:指出可持續土地利用是將技術、政策和旨在使社會經濟原理與環境關系一體化行為結合起來,以便同時達到保持或提高生產或服務,降低生產風險,保持自然資源潛力和防止土退化,使其具有經濟活力和被社會所接受。
  10. Experimental studies were conducted at the yucheng comprehensive experimental station of the chinese academy of sciences during the period from march to june in 2003. respiration of a pulverous sandstone soil was studied under cultivation of winter wheat over a growth season. soil ch4 was measured by the static - chamber method combined with gas chromatography ( gc ) technique. the results indicated that the soil of winter wheat field in rapid growth season is a weak sink of ch4

    本文利用靜態箱氣相色譜( gc )分析的方法,在中國科學院禹城綜合試驗站,對華北平原冬小麥生長旺季期間麥田土中ch _ 4氣體通量進行了測定,試驗起止時間為2003年3 6,得出華北平原典型冬麥田土是大氣ch _ 4的弱吸收匯。
  11. Finally, nasa and the florida space research institute are sponsoring moonrox, the moon regolith oxygen competition. a 250, 000 prize goes to the team that can extract 5 kg of breathable oxygen from jsc - 1 lunar stimulant, a new lunar soil simulant developed under the auspices of nasa johnson space centre, in 8 hours

    最後,美國太空總署和佛羅里達太空研究中心,正贊助一項名為球表土氧氣的賽事,提供25萬美元獎金給率先在八小時內能從美國太空總署莊臣太空中心的模擬球土jsc - 1提取5公斤可呼吸氧氣的人。
  12. Both soil seed banks and seed movement showed seasonal variation, and usually reached the maximum in october

    種子庫和表面種子流表現出季節性動態變化,均在10份達到最大。
  13. Abstract : soil incubation experiments were conducted in lab to delineate the effect of soil temperature and soil water content on soil respirations in broad - leaved / korean pine forest ( mountain dark brown forest soil ), dark coniferous forest ( mountain brown coniferous forest soil ) and erman ' s birch forest ( mountain soddy forest soil ) in changbai mountain in september 2001. the soil water content was adjusted to five different levels ( 9, 21, 30, 37 and 43 ) by adding certain amount of water into the soil cylinders, and the soil sample was incubated at 0, 5, 15, 25 and 35 for 24 h the results indicated that in broad - leaved / korean pine forest the soil respiration rate was positively correlated to soil temperature from 0 to 35. soil respiration rate increased with increase of soil water content within the limits of 21 to 37, while it decreased with soil water content when water content was over the range. the result suggested the interactive effects of temperature and water content on soil respiration. there were significant differences in soil respiration among the various forest types. the soil respiration rate was highest in broad - leaved / korean pine forest, middle in erman ' s birch forest and the lowest in dark coniferous forest. the optimal soil temperature and soil water content for soil respiration was 35 and 37 in broad - leaved / korean pine forest, 25 and 21 in dark coniferous forest, and 35 and 37 in erman ' s birch forest. because the forests of broad - leaved / korean pine, dark coniferous and erman ' s birch are distributed at different altitudes, the soil temperature had 4 - 5 variation in different forest types during the same period. thus, the soil respiration rates measured in brown pine mountain soil were lower than those in dark brown forest and those measured in mountain grass forest soil were higher than those in brown pine mountain soil

    文摘:為了研究土溫度和土含水量對闊葉紅松林(山地暗棕) 、雲冷杉暗針葉林(山地棕針葉林土)和岳樺林(生草森林土)的土呼吸的影響,於2001年9在長白山進行了土實驗.利用增加土樣柱的含水量,將土含水量分為9 , 、 21 、 30 、 37和43 5個等級,土樣品分別在0 、 5 、 15 、 25和35的溫度下保持24小時.闊葉紅松林土在0 ( 35范圍內,土呼吸速率與溫度呈正相關.在一定的含水量范圍內( 21 ( 37 ) ,土呼吸隨含水量的增加而升高,當含水量超出該范圍,土呼吸速率則隨含水量的變化而降低.土溫度和水分對土呼吸作用存在明顯的交互作用.不同森林類型土呼吸作用強弱存在顯著差異,大小順序為闊葉紅松林>岳樺林>雲冷杉暗針葉林.紅松闊葉林土呼吸作用的最佳條件是土溫度35 ,含水量37 ;雲冷杉暗針葉林下的山地棕色針葉土呼吸作用的最佳條件是25 , 21 ;岳樺林土呼吸作用的最佳條件是35 ,含水量37 .但是,由於長白山闊葉紅松林,雲冷杉林和岳樺林處在不同的海拔帶上,同期不同森林類型土溫度各不相同,相差4 ~ 5 ,所以野外所測的同期的山地棕色針葉林土呼吸速率應低於暗棕色森林土呼吸速率,山地生草森林土呼吸速率應高於山地棕色針葉林土的呼吸速率.圖2表1參25
  14. Soil incubation experiments were conducted in lab to delineate the effect of soil temperature and soil water content on soil respirations in broad - leaved / korean pine forest ( mountain dark brown forest soil ), dark coniferous forest ( mountain brown coniferous forest soil ) and ermans birch forest ( mountain soddy forest soil ) in changbai mountain in september 2001. the soil water content was adjusted to five different levels ( 9, 21, 30, 37 and 43 ) by adding certain amount of water into the soil cylinders, and the soil sample was incubated at 0, 5, 15, 25 and 35 for 24 h the results indicated that in broad - leaved / korean pine forest the soil respiration rate was positively correlated to soil temperature from 0 to 35. soil respiration rate increased with increase of soil water content within the limits of 21 to 37, while it decreased with soil water content when water content was over the range. the result suggested the interactive effects of temperature and water content on soil respiration. there were significant differences in soil respiration among the various forest types. the soil respiration rate was highest in broad - leaved / korean pine forest, middle in ermans birch forest and the lowest in dark coniferous forest. the optimal soil temperature and soil water content for soil respiration was 35 and 37 in broad - leaved / korean pine forest, 25 and 21 in dark coniferous forest, and 35 and 37 in ermans birch forest. because the forests of broad - leaved / korean pine, dark coniferous and ermans birch are distributed at different altitudes, the soil temperature had 4 - 5 variation in different forest types during the same period. thus, the soil respiration rates measured in brown pine mountain soil were lower than those in dark brown forest and those measured in mountain grass forest soil were higher than those in brown pine mountain soil

    為了研究土溫度和土含水量對闊葉紅松林(山地暗棕) 、雲冷杉暗針葉林(山地棕針葉林土)和岳樺林(生草森林土)的土呼吸的影響,於2001年9在長白山進行了土實驗.利用增加土樣柱的含水量,將土含水量分為9 , 、 21 、 30 、 37和43 5個等級,土樣品分別在0 、 5 、 15 、 25和35的溫度下保持24小時.闊葉紅松林土在0 ( 35范圍內,土呼吸速率與溫度呈正相關.在一定的含水量范圍內( 21 ( 37 ) ,土呼吸隨含水量的增加而升高,當含水量超出該范圍,土呼吸速率則隨含水量的變化而降低.土溫度和水分對土呼吸作用存在明顯的交互作用.不同森林類型土呼吸作用強弱存在顯著差異,大小順序為闊葉紅松林>岳樺林>雲冷杉暗針葉林.紅松闊葉林土呼吸作用的最佳條件是土溫度35 ,含水量37 ;雲冷杉暗針葉林下的山地棕色針葉土呼吸作用的最佳條件是25 , 21 ;岳樺林土呼吸作用的最佳條件是35 ,含水量37 .但是,由於長白山闊葉紅松林,雲冷杉林和岳樺林處在不同的海拔帶上,同期不同森林類型土溫度各不相同,相差4 ~ 5 ,所以野外所測的同期的山地棕色針葉林土呼吸速率應低於暗棕色森林土呼吸速率,山地生草森林土呼吸速率應高於山地棕色針葉林土的呼吸速率.圖2表1參25
  15. Its soil contains raw materials that might be harvested and processed into rocket fuel or breathable air

    球土包含的原材料可以被採集和加工成飛船燃料或者可以呼吸的空氣。
  16. A transfer model is established, which can be used to study the interaction between the land surface physical processes of inhomogeneous region and the structure of atmosphere boundary - layer over urban and rural terrains. the model has simulated surface heat flux, surface temperature, temperature profiles, height of mixture layer and so on. and the differences between urban area, suburban area and rural area have been compared. this model mainly depends on the parameters below : surface albedo, surface roughness coefficient, moisture available coefficient of soil, thermal capacity and thermal diffusion coefficient of errain, cloudage. the result shows that this model can simulate the structure and eigenvalues of atmosphere boundary layer and their changes in a day. parameters used in this model aim at beijing city, and the time is at the beginning of september. to other cities, or other time, the parameters should be adjusted accordingly. in addition, being adjusted, the model can also be used for other homogeneous and inhomogeneous terrains

    模式主要依賴于以下參數和物理量:地面反照率下墊面粗糙度土的可含水量下墊面的熱容量和熱擴散系數雲量等參數。結果表明,本模式能合理地模擬不同地表熱量平衡地表氣溫混合層高度湍流交換系數湍流動能位溫廓線等,以及它們的日變化。該模式所取參數主要針對北京市,時間為九初,對于其他城市,參數應作相應的調整。
  17. It was a great comfort to me afterwards, that i did so, for not one grain of that i sow d this time came to any thing ; for the dry months following, the earth having had no rain after the seed was sown, it had no moisture to assist its growth, and never came up at all, till the wet season had come again, and then it grew as if it had been but newly sown

    值得慶幸的是,我做對了。我這回下的種子,一顆也沒長出來。因為種子下地之後,一連幾個不下雨,土里沒有水份,不能滋潤種子生長,一直到雨季來臨才冒了出來,好像這些種子剛播種下去似的。
  18. Lunar surface can be regarded approximately as two - layered medium composed of lunar soil and lunar rock. therefore, in this paper, two - layered medium is mainly discussed

    球表層可近似視為由月壤巖組成的雙層結構,因此,本文主要針對雙層媒質進行討論。
  19. The aim of this paper is to find a method to estimate the thickness of lunar soil from the values measured by lunar microwave radiometer

    本文的主要目的是尋找一種反演方法,利用球探測衛星微波輻射計的亮度溫度數據評估月壤厚度。
  20. A review and prospect for developing of lunar soil simulants

    模擬月壤研製的初步設想
分享友人