1)yellow soil黄壤
1.Strontium isotopes as a tracer of plant nutrition element source in yellow soil region of Guizhou Province;贵州黄壤地区植物营养元素来源的Sr同位素示踪
2.Study on the nutrients characteristic in mountain yellow soil of Chongqing baced on the mathod of principal component analysis and cluster analysis;重庆市山地黄壤养分特性的主要成分和聚类分析
3.N-loss of ammonia-volatilizing from urea applied in both red soil and yellow soil with the rotation of Digitaria ischaemum in spring and winter radish in autumn;春季马唐-秋季冬萝卜红壤和黄壤中尿素氨挥发损失状况的研究
英文短句/例句
1.From the foot to the top of Jinfo Mountain, the soils appear as yellow soil, dark yellow soil, yellow brown soil and brown soil.土壤分带性主要表现为：从山下向山顶依次为黄壤、暗黄壤、黄棕壤和棕壤。
2.c)Among various soil types,erosion on yellow soil and lime soil is most prominent,besides them are red soil,yellow brown soil,paddy soil,brown soil,dark brown forest soil,laterite soil,brown soil,lateritic red soil and black clay soil.在各种土壤类型中,黄壤和石灰土的土壤侵蚀最为突出,其次为红壤、黄棕壤和南方水稻土等;
3.MORPHOLOGICAL CHARACTERISTICS OF MAJOR CLAY MINERALS IN RED SOIL,LATERITIC RED SOIL AND YELLOW SOIL IN FUJIAN福建红黄壤主要粘粒矿物的形态特征
4.Spatio-temporal Variation of Soil Moisture in Sloping Land of Guizhou Yellow Soil贵州坡地黄壤水分时空变异特征研究
5.The Study on Residue Trends of Fonofos in Red Soil and Yellow Brown Soil地虫硫磷在红壤与黄棕壤中的残留动态研究
6.The Study on the Basic Attributes and Quantitative Distinctive Indexes between Brown Soil and Yellow Brown Soil棕壤和黄棕壤基本属性及定量区分指标的研究
7.Effect of Soil Erosion on Soil Organic Carbon in Chinese Loess Plateau;黄土高原坡耕地土壤侵蚀对土壤有机碳的影响
8.The Influence of Soil Erosion and Soil Fertility on Planting Coptis Chinensis;黄连种植对土壤侵蚀及土壤肥力的影响研究
9.Comparitive Study upon Soil Erosion Processes on Red Soil Hillslope and Loess Hillslope红壤坡面与黄土坡面土壤侵蚀过程对比研究
10.Influence of Soil Particle Composition on Soil Moisture in Loess Profiles黄土剖面土壤颗粒组成对土壤含水量的影响
11.Fractal characteristics of soil particle composition for typical types of soil profile on Loess Plateau黄土高原典型土壤剖面土壤颗粒组成分形特征
12.Clay mineral composition and surface charge characteristics of red earth and yellow brown earth were studied.本文研究了红壤与黄棕壤的粘粒矿物组成与土壤的表面电荷特征。
13.The Diagnostic Properties and Diagnostic Indexes of Yellow Brown Earth and Cinnamon Soil in the South Part of Shaanxi陕南黄棕壤、黄褐土诊断特征及诊断指标的研究
14.Sand and dust covered the sky of Pyongyang and Seoul; yellow sand everywhere in the Korean peninsula朝鲜半岛黄沙蔽日 平壤汉城灰尘遮天
15.Fertilizer Effects on Wheat in Pot with Xinzhou Yellow Brown Earth新洲黄棕壤盆栽小麦肥料效应的研究
16.Application of Jute Geotextile for Controlling Soil Erosion黄麻土工布在土壤侵蚀控制中的应用
17.Effect of Jute Geotextiles on Soil Anti-erodibility黄麻土工布对土壤抗侵蚀性能的影响
18.On some Chemical and Physical properties of Salt-affected Soils in Yellow River(Gansu Section)lrrigation Areas;甘肃沿黄灌区盐化土壤理化性质研究
相关短句/例句
acid yellow soil酸性黄壤
1.Characteristics of Pb absorption and accumulation by tomato in acid yellow soil;番茄对酸性黄壤中铅的吸收特性与富集效果
3)Yellow brown soil黄棕壤
1.Pot experiments were conductedand plant analysis was made to study the effects of Cd and Pb on the growth of lettuce and its heavy metal uptake when growing in polluted yellow brown soil.用盆栽试验结合化学分析研究了黄棕壤中镉(Cd)、铅(Pb)复合污染对莴苣生长、品质及重金属元素吸收的影响。
2.And the soil vertical distribution is in the order of yellowcinnanon soil (<900 m),yellow brown soil ( 900.大巴山北坡基带土壤为黄褐土（＜９００ｍ），自下而上依次分布着黄棕壤（９００～１６００ｍ）、棕壤（１６００～２６００ｍ）、暗棕壤（＞２６００ｍ）。
4)Yellow brown earth黄棕壤
1.The characteristics of adsorption-desorption of Cd in yellow brown earth with pH;不同pH下黄棕壤镉的吸附-解吸特征
2.The adsorption of Cu2+by four typical soils--latersol, red l atersol, yellow brown earth and dark brown earth of China were measured under si ngle and coexisting Na+,Ca2+or Zn2+conditions, respectively.采用室内试验方法,研究了我国4种典型土壤——砖红壤、赤红壤、黄棕壤和暗棕壤在伴随阳离子分别为Na+、Ca2+、Zn2+时对Cu2+的吸附。
5)sloping field of yellow soil坡地黄壤
6)yellow soil slope region黄壤坡地
1.Soil microelements under different vegetation restoration patterns in yellow soil slope region of mid-subtropics.;不同植被恢复模式下中亚热带黄壤坡地土壤微量元素效应
2.In the case of Nverzhai watershed in Wulin mountain region,community structures of Machilus pingii secondary forestry were studied in the yellow soil slope region of middle subtropics,which included vertical layer structure,distribution patterns of dominant populations and DBH & height structure of tree layer.为了探讨中亚热带侵蚀黄壤坡地植被恢复模式的群落结构,以武陵山区女儿寨小流域为例,运用群落生态学的研究方法对润楠次生林的垂直层次结构、种群水平分布格局、乔木层直径与树高分布结构进行了研究。
延伸阅读
黄壤黄壤yellowearth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。黄壤剖面
