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   character of soil 在 自然地理学和测绘学 分类中 的翻译结果: 查询用时:0.565秒
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character of soil
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  土壤性质
    Basin simulating experiment was adopted to study the character of soil after decomposition of Chinese fir leaf litter mixed with Phoeba bournei and Schima superba. The results showed that the percentage of bacteria to all microbe was from 98.19 to 99.80%,the percentage of fungi to actinomycetes was from 0.12 to 1.01% and from 0.12 to 1.08%,respectively;
    通过盆钵模拟试验对杉木与楠木、杉木与木荷叶凋落物混合分解后土壤性质进行研究,结果表明:土壤微生物区系中,细菌占微生物总数的98.18%~99.80%,真菌、放线菌在微生物总量中的比例差异不显著(P>0.05),分别为0.12%~1.01%和0.12%~1.08%;
短句来源
  土壤性质
    Basin simulating experiment was adopted to study the character of soil after decomposition of Chinese fir leaf litter mixed with Phoeba bournei and Schima superba. The results showed that the percentage of bacteria to all microbe was from 98.19 to 99.80%,the percentage of fungi to actinomycetes was from 0.12 to 1.01% and from 0.12 to 1.08%,respectively;
    通过盆钵模拟试验对杉木与楠木、杉木与木荷叶凋落物混合分解后土壤性质进行研究,结果表明:土壤微生物区系中,细菌占微生物总数的98.18%~99.80%,真菌、放线菌在微生物总量中的比例差异不显著(P>0.05),分别为0.12%~1.01%和0.12%~1.08%;
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  “character of soil”译为未确定词的双语例句
    Type and Character of Soil Degradation and Sustainable Agriculture in Fujian Province
    福建土壤退化类型、特征与持续农业
短句来源
    2. The basics character of soil profile salinization was showed as follow: the 0-40cm layer was the category of sulfate-chloride and salt content variance 0.058%-0.073%;
    2.土壤剖面盐渍化基本特征是:0-40cm土层属硫酸盐-氯化物类型,盐分含量变异在0.058%-0.073%;
短句来源
    (2) It was very effective to describing the character of soil particle distribution by using multi-fractal method.
    (2)应用多重分形的方法来描述土壤粒径分布性质是非常有效的。
短句来源
    3) cultivate the parent material inoculated fungus(and their mixture), discussed the function of the microbe to the formation and character of soil humus substance.
    3)母质中接种真菌微生物(青霉、木霉、曲霉及其混合茵)培养,探讨微生物对土壤腐殖物质形成及性质的作用意义。
短句来源
    Through imitating the feature curve of soil moisture of different stand, we know the character of soil moisture of different stand, and through classifing to soil moisture, we calculate the effective value of soil moisture of different stand.
    运用先进的研究手段对不同林分的土壤的持水性能进行研究,通过对土壤水分特征曲线的拟合,掌握不同林分比水容量特征,并对不同林地的土壤水分进行分类,计算出不同林地土壤水分有效性的临界点,从而求出不同林地的有效水范围。
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  character of soil
Effect of local loads on the character of soil pressure on productive structures
      
The character of soil generation in this area is influenced by the frigid, coniferous forest vegetation, weather, glacier and late soil formation process.
      
A preliminary analysis is made of the change in character of soil formation in regraded and postagrogenic soils.
      
It is suggested that information on the genetic diversity of soils, their properties, and the character of soil management should be specially collected and systematized in order to make strategic decisions aimed at soil conservation.
      
Litter samples from peat podzolic (Stagnic Podzoluvisol) and soddy gley (Mollic Gleysol) soils differing in their chemical and physicochemical properties, geochemical conditions, and the character of soil microbial complexes were analyzed.
      
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Shergyla Mountain is situated in the Southeast Xizang and is one of the main forest zone in Xizang. By the changes of climate and forest,the vertical belts of mountain soil type are guite clear. There is the mountain brown forest soil at the base,and as the elevation rising,there are mountain acid brown forest soil, mountain bleached podolic soil, subalpine (shrubs) marshland soil,alpine marshland soil and alpine wilderness soil in proper order,and they are distributed...

Shergyla Mountain is situated in the Southeast Xizang and is one of the main forest zone in Xizang. By the changes of climate and forest,the vertical belts of mountain soil type are guite clear. There is the mountain brown forest soil at the base,and as the elevation rising,there are mountain acid brown forest soil, mountain bleached podolic soil, subalpine (shrubs) marshland soil,alpine marshland soil and alpine wilderness soil in proper order,and they are distributed symmetrically on the east and west slopes. The vertical distributionlaw of texture regime, organic matter and soil nutrient,pH or soil, composition of exchangeable and chemical comporition is discussed. The results are:1. Among the mount at 4 000 (3 700m east slope)-4 200m,there are clear podzolic layer, and the main cause to form is that the vegetation is thick, the air is damp, surface organic matter increases and the leaching action strengthens, then the most of Fe and Al runs off and the Si gathes.2. The vertical distribution of mount soil is clear,but the characters of each soil type are very different,for example,the organic matter make up 9 to 373g/kg,pH of soil expresses strong acid reaction to strong alkaline reaction, the base is saturated to not saturated highly. Especially podzolic soil,its many characters in the vertical distribution are very abnormal.3. At the same section, the regulars of each type soil in vertical distributtion are same almost. From top to deep soil,the characters of soil tend to primitive state,but the characters of podzolic soil are very different at the different places.4. The types of soil on the east and west slopes at the same elevation belt are identical basically and distribution symmetrically, but the characters of soil are different slightly. Generally, because that the rainfall is high and the growth of vegetation is well on the east slope, the appearance of leaching of soil on the east slope is more clear than on the west slope5. There is the special soil in same areas. By the difference with vegetation and condition of soil forming,the soil charactersare very different to the others at same belt.

色季拉山位于青藏高原的东南部,是西藏主要林区之一。由于气候和森林的垂直变化,其山体土壤类型的垂直带谱较为明显,基带为山地棕壤,往上依次为山地酸性棕壤、山地漂灰土、亚高山(灌丛)草甸土(黑毡土、棕毡土)、高山草甸土(草毡土)和高山寒漠土,并且东西坡呈对称分布。在分析了各类土壤的特征之后,讨论了土壤质地、有机质与养分、pH值、交换性能及化学组成的垂直分布规律。

The particle composition, pH and organic carbon content of agricultural soil of north basin of Baiyangdian Lake were determined with standard methods in the paper, and the character of soil was studied using comparison method. The results show that the pH of surface soil is 8.318.77 and has mean value of 8.49 which does not have distinct variation to compare with 10 years ago; the organic carbon content is 0.77%1.21% and has a mean value of 0.96% which is 1.26 time of 10 years ago; sandy soil...

The particle composition, pH and organic carbon content of agricultural soil of north basin of Baiyangdian Lake were determined with standard methods in the paper, and the character of soil was studied using comparison method. The results show that the pH of surface soil is 8.318.77 and has mean value of 8.49 which does not have distinct variation to compare with 10 years ago; the organic carbon content is 0.77%1.21% and has a mean value of 0.96% which is 1.26 time of 10 years ago; sandy soil is main composition of studied soils. The results of vertical sample determination show that pH increases with soil column vertical depth and the organic carbon content is decreases with vertical depth.

本文采用标准方法,测定了白洋淀北岸部分农田土壤的粒度组成、pH和有机碳含量等指标,对该地区土壤的特性进行了表征分析。结果表明,土壤的平均粒度分布大于20μm的占52.73%,主要属于砂壤土。与10年前相比,pH值变化不大;而有机碳含量是10年前的1.26倍。pH随土壤的垂直深度而略有增加,而有机碳含量则随土壤的垂直深度而减少。

According to the nature, Guangxi Limestone is separated into three types:pure limestone, siliceous limestone, mixed sand shale or limestone of igneous rock. Thephysical and chemical characters of soil, which is formed by different limestone weatheringand developing, are notable diversity. These have great effect on agricultural production.Only when we suit measures to local conditions, arrange rationally production of agriculture, forestry and animal husbandry can we obtain good economic, social, ecological...

According to the nature, Guangxi Limestone is separated into three types:pure limestone, siliceous limestone, mixed sand shale or limestone of igneous rock. Thephysical and chemical characters of soil, which is formed by different limestone weatheringand developing, are notable diversity. These have great effect on agricultural production.Only when we suit measures to local conditions, arrange rationally production of agriculture, forestry and animal husbandry can we obtain good economic, social, ecological andsynthesized benefit.

广西的石灰岩按性质可分为纯质石灰岩、夹硅质石灰岩、夹砂页岩或火成岩的石灰岩三种类型。不同的石灰岩风化发育形成的土壤的理化性质差异显著,对农业生产的影响巨大,必须因地制宜,合理安排农、林、牧业生产,才能取得良好的经济、社会和生态的综合效益。

 
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