1) cultivated loess
耕淀黄壤
2) sloping farming land of yellowish red soil
红黄壤坡耕地
3) cultivated soil
耕作土壤
1.
Heavy metals contamination for cultivated soils,vegetables and rice in the vicinity of non-ferrous metals industry;
有色矿业区耕作土壤、蔬菜和大米中重金属污染
2.
Study on potassium release rate and the relation of the rate to potassium availability in Cultivated soils;
耕作土壤释钾速率及其与钾有效性的关系研究
3.
Spatial autocorrelation analysis of heavy metals in cultivated soils in Beijing
北京耕作土壤重金属含量的空间自相关分析
4) Cultivated land
耕地土壤
1.
Changing trend of organic matter and nutrient content in cultivated land of the Ningxia irrigation area of yellow river;
宁夏引黄灌区耕地土壤有机质及养分质量分数变化趋势
2.
It has been 20 years since the Second Soil Census,in order to know the dynamic change of soil phosphorus,the data of soil phosphorus in cultivated land in Ankang from 1995 to 2003 is analyzed and the result is compared with the Second Soil Census.
第二次土壤普查迄今已20年,为了摸清土壤磷素的变化动态,对安康市1995～2003年耕地土壤有效磷化验资料进行了统计分析,并与第二次土壤普查结果进行了比较研究,结果表明,土壤有效磷呈上升趋势,严重缺磷土壤减少,但中高山地区土壤缺磷依然严重。
5) Cultivated soil
耕地土壤
1.
Study on Cu content in cultivated soils and its influence factors in Guangxi;
广西耕地土壤铜的含量及其影响因素
2.
Geostatistical methods were used in combination of GIS to analyze the spatial distribution characteristics of total K and available P in cultivated soils in Xinhui district,Guangdong Province,over 20 years from 1982 to 2003.
结果表明,研究区域耕地土壤由于20年来的耕作施肥使得土壤全钾和有效磷含量显著增加,土壤全钾在研究区域的南部变化最明显,与该地区的土壤类型为咸田有很大关系;耕地土壤全钾和有效磷的空间分布都表现为中等空间相关性;土壤全钾和有效磷变程的变化与土壤养分在土壤中化学行为有关。
3.
In this project, analytical data of 20 items from 367 of cultivated soil samples in Minhou county were selected, and principle component and gray relation analysis methods were used for revealing the relationship between soil properties and environmental factors.
耕地土壤性质与气候、地形、母质等自然环境和人类活动存在错综复杂的内在联系 。
6) plough layer
土壤耕层
1.
By simulating the movement of groundwater in soil plough layer, the pollution characters of groundwater contaminated by salinity and heavy metals in the plough layer were researched under different water tables, different pollution levels and various texture soils.
通过模拟不同水位、污染度的地下水在不同质地土壤耕层中的迁移,进行了地下水中盐分和重金属对土壤耕层污染规律的研究。
补充资料：黄壤
| 黄壤 yellow earth 发育于亚热带湿润山地或高原常绿阔叶林下的土壤。酸性，土层经常保持湿润，心土层含有大量针铁矿而呈黄色，故名。集中分布于南北纬度23.5°～30°之间。中国主要分布于四川、贵州等省，为南方山区的主要土壤类型。在山地的垂直带谱中，黄壤下部一般是红壤，上部以黄棕壤为多。黄壤的形成包含富铝化作用和氧化铁的水化作用两个过程。由于高温多雨、岩石风化强烈，在成土过程中难移动的铁、铝在土壤中相对增多；土壤终年处于相对湿度大的环境中，土体中大量氧化铁发生水化作用而形成针铁矿。黄壤分为3个亚类：①黄壤。多见于原生植被保存较少，次生栎类灌丛和稀疏马尾松、杉木混交林较多的山地，有机质含量随自然植被的不同而有很大差异。②灰化黄壤。多见于海拔较高、森林保存较好、郁闭度较大的地段，有明显的枯枝落叶层，表土呈强酸性，有机质含量达10％以上。③表潜黄壤。多见于亚热带山地的山脊地带，常年云雾弥漫，相对湿度较大，有较厚的枯枝落叶层，表层水分常呈饱和状态而有滞水现象，表层有机质含量达20％左右。黄壤的利用以多种经营为宜。已耕种的黄壤为防止土壤侵蚀，宜进行农田基本建设，多施有机肥和种植绿肥，并适量施用石灰和磷肥。
|
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条