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1)  red soil erosion
红壤孔隙
2)  soil porosity
土壤孔隙
1.
The results showed that:(1)The soil water infiltration rates in layer A were higher than those in layer B for all kinds of vegetation,which were remarkably related to soil porosity.
结果表明:(1)各森林植被类型林地A层土壤渗透速率和孔隙度均高于B层,土壤渗透速率与土壤孔隙度之间存在显著相关关系。
3)  soil macropore
土壤大孔隙
1.
Soil macropore and its studying methodology.;
土壤大孔隙及其研究方法
2.
The soil macropore could contain some preferential flow, which would lead to groundwater pollution.
土壤大孔隙可导致优先流从而引起地下水污染,植物根孔属于土壤大孔隙的一类,它在导致优先流引起的地下水污染方面有特殊的作用。
4)  pore water of soil
土壤孔隙水
5)  soil porosity
土壤孔隙度
1.
By analysis of sampled soil physical properties,compared that with bare area,the results show that: there is no certain change pattern between soil bulk density and soil porosity;the bulk of soil bulk density gets larger and the soil gets deeper,while the soil bulk density gets smaller at certain depth and the capability of sluice falls.
以徐州市三环路内4个城区的公园绿地土壤为研究对象,通过对其土壤的物理性状取样分析,同时与无植被覆盖的裸地进行对比,结果表明:该城区公园绿地土壤容重与孔隙度随时间无确定的变化规律;该土壤容重开始随土壤深度增加而减小,某一深度以后逐渐增加,而土壤孔隙度随土壤深度增加而增加,某一深度以后逐渐减小,土壤蓄水保水能力降低。
2.
Plastic mulching or intercropping combined with pruning and fertilization not only increased the biomass yield of Japanese honesuckle ( Lonicera japonica Thumb) but also improved its water- and soil-conserving effect, for such management technologies decreased soil bulk density, increased soil porosity and enhanced the water-holding capacity of the soil.
对金银花采取地膜覆盖、间作的种植模式,结合修剪、施肥的管理技术,可有效降低土壤容重,增加土壤孔隙度,提高土壤贮水量,不仅增加了金银花的生物学产量,而且提高金银花的水土保持效益。
3.
The results showed the evident existences of the vertical spatial variability of porosity in soils on mm-scale; the variability of the cultivated soil originated from a prairie soil was higher than that originated from a forest soil, and the variability has a negative relation with the soil porosity but a positive relation with the soil depth with the tillage horizon; however, the variabi.
结果表明,土壤孔隙度在 mm尺度上存在较为明显的变异;不同的土壤变异性存在一定的差异;变异性与土壤孔隙度呈反向关系,与土壤深度呈正向关系;在耕作期,变异性随时间呈现一定的波动趋势。
6)  soil pores
土壤孔隙 SP
补充资料:红壤
红壤
red earth

   发育于热带和亚热带雨林、季雨林或常绿阔叶林植被下的土壤。主要特征是缺乏碱金属和碱土金属而富含铁、铝氧化物,呈酸性红色。主要分布于非洲、亚洲、大洋洲及南北美洲的低纬度地区。大致以南北纬30°为限。在中国,北起长江沿岸,南抵南海诸岛,东自台湾省,西至云贵高原及横断山脉为主要分布区域。红壤的形成是在高温多雨、植被茂密的生物、气候条件下,土壤中富铝化和生物富集相互作用的结果。根据成土条件的变化和富铝化作用的强度,中国境内红壤可分为砖红壤、砖红壤性红壤、红壤、黄壤4个亚类。前2类多见于热带和南亚热带,土体中碱金属及碱土金属含量均低,pH4.5~5.0,适宜种植热带和亚热带作物及水稻。第3类多见于亚热带低山丘陵地带,土壤pH5.0左右,富铝化程度较前2类弱,适宜种植亚热带经济作物和水稻、玉米等。为更好地利用红壤,须对其淋溶作用强、矿质养分少、酸性大、易产生铝锰毒害、保肥性能差和质地粘重或砂粒过多等不良性状进行改良。具体措施是:增施氮、磷、钾等矿质肥料,氮肥宜用粒状或球状深施,磷肥宜与有机肥混合制成颗粒肥施用;施用石灰降低土壤酸性;合理耕作;选种适当的作物、林木,种植绿肥是改良红壤的关键措施;旱地改水田,减少水土流失并有利于有机质积累,提高土壤生产力;保护植被,防治侵蚀,凡坡度大于25°的陡坡应以种树种草为主,小于25°的坡地根据陡缓状况修建宽窄不等的等高梯地或梯田种植。
   
   

红壤剖面

红壤剖面

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