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meadow brown相关的网络例句

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For actual productivity of soybean, the rank is black soil, meadow soil, dark brown soil, chernozem saltierra and saltern, aeolian soil.

不同土壤条件下的大豆现实生产力存在差异:黑土>草甸土>暗棕壤>黑钙土和盐碱土>风沙土。

For different soils, the rank of actual productivity of maize is black soil, meadow soil, chernozem dark brown soil saltierra and saltern, aeolian soil.

不同类型耕作土壤对玉米和大豆现实生产力的影响分析表明,对于玉米而言,6类不同土壤条件下的玉米现实生产力存在以下规律:黑土>草甸土>黑钙土、暗棕壤和盐碱土>风沙上。

Zonal soils chestnut brown calcium soil and soil small size, only the upper part of the distribution of the alluvial fan and central parts of the formation of long-term irrigation Yuguan light meadow soil widespread development, soil depth, with certain fertility, is a good base for grain production.

地带性土壤栗钙土和棕钙土面积不大,仅分布在洪积扇的上部和中部,长期灌溉形成的淤灌浅色草甸土广泛发育,土层深厚,具有一定肥力,是粮食生产的良好基地。

County soil parent material is limestone, sandstone, gneiss evolved over the three types of rock, soil can be divided into four categories, namely, mountain meadow soil, mountain brown, cinnamon, meadow soil, Cinnamon Is the backbone of the county soil.

全县土壤母质是由石灰岩、沙岩、片麻岩三类母岩演变而成的,可分为四个土类,即山地草甸土、山地棕壤、褐土、草甸土,褐土是全县的骨干土壤。

In this study the meadow brown soil in northeast China was picked up as the object, through the research of Sn, Hg, Sb, and Bi desorption kinetics behavior in single and combined polluted soils we explored the desorption characters and rules of Sn, Hg, Sb, and Bi in polluted soils.

文章以我国东北地区草甸棕壤作为研究对象,通过对Sn、Hg、Sb、Bi单一及复合污染土壤中Sn、Hg、Sb、Bi的解吸动力学行为的研究,探索污染土壤中重金属Sn、Hg、Sb、Bi的解吸特性与规律。

According to the values of pHPZNC, N s and structural negative charge density measured, the intrinsic surface reaction equilibrium constants, p K of 1-p K model, p K a1int and p K a2int of 2-p K model, were directly calculated to be 3.37, 2.42 and 4.32, respectively, for the meadow brown soil in northeast of China.

根据实验测定的pHPZNC, N s和结构电荷密度值直接计算得出东北草甸棕壤样品的界面反应特征平衡常数即1-p K 模型中的p K , 2-p K 模型中p K a1int和p K a2int,分别为3.37, 2.42和4.32,与文献报道的沉积物和蒙脱土的值相吻合。

Among the environmental factors,temperature nearly make the same effect toall the tree species of broad leaf korean pine forest.Moisture and fertility of soil aregreatly depend on the soil type.In the broad leaf korean pine forest zone,humus darkbrown soil has the best condition of moisture and fertility,The following are typicaldark brown soil、flood and forest soil;the third is albic brown soil and meadow soil;The worst ones are skeleton brown soil and marshy soil.

在影响树木生长的环境因子中,温度对所有树木的影响几乎相同,土壤的水肥因子是与土壤类型相关性很大的量,不同的土壤类型,水肥条件相差极大,在长白山阔叶红松林带,土壤水肥条件最好的是腐殖质暗棕壤,其次是典型暗棕壤和河滩森林土,土壤水肥条件一般的是草甸土和潜育暗棕壤,水肥条件最差的是粗骨棕壤和沼泽土。

Using a coated urea (Polyolefin-coated urea, 70 day, POCU) made in Japan and a conventional granular urea as check nitrogen release characteristics of four kinds urea amended with biological inhibitor and coated or coated by acrylic resin fertilizers in Meadow Brown Soil are examined under constant temperature incubating in laboratory.

在室内恒温培养条件下,以日本70 d聚烯烃包膜尿素和大颗粒尿素为对照,研究4种丙烯酸树脂包膜及其与生化抑制剂结合尿素肥料在土壤中尿素态氮溶出与水解特征,以确定不同种MMA包膜尿素在土壤中缓/控释效果与尿素转化机理。

Compared carbon pools and turnovertime under different soil types, the result shows: soil total organic carbon is grey cinnamonforest soil>dark-brown soil>meadow soil>brown coniferous forest soil>red soil>yellowsoil>yellow brown soil>paddy soil>red soil>flubo-aquic soil>fengsha soil,temperate forest soil>subtropical forest soil>subtropical cropland soil>temperate dry soil.Active carbon is temperate forest soil>subtropical soil.

对不同土壤类型的碳库及其驻留时间进行比较,得出:有机碳含量呈现:灰褐土>暗棕壤>草甸土>棕色针叶林土>红壤>黄壤>黄棕壤>水稻土>农田红壤>潮土>风沙土,温带森林土壤>亚热带森林土壤>亚热带农田土壤>温带干旱土壤;活性碳含量是温带森林土壤>亚热带的土壤。

Qilian Mountains are mainly located in the mountains for a cold desert soil → ash swamp land and soil; Long in the first mountain chestnut soil as a soil-gray →→ gray-brown desert soil; in the northern Gobi desert soil as a gray-brown sand of a wind →→ saline soil; corridor oasis for irrigated desert soil → a gray-brown desert soil of a meadow → soil.

在祁连山区主要分布为高山寒漠土一→灰钙土及沼泽土;龙首山区为栗钙土一→灰钙土一→灰棕漠土;北部戈壁为灰棕漠土一→风沙土一→盐土;走廊绿洲为灌漠土一→灰棕漠土一→草甸土。

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