1) Newly cultivated lateritic red soil
新垦赤红壤
2) new reclaimed red soil
新垦红壤
1.
Effects of green manure,chicken manure,and calcium fertilizer application on soil fertility and flue-cured tobacco growth in a new reclaimed red soil;
绿肥、鸡粪和钙肥使用对新垦红壤土壤肥力和烟草生长的影响
3) Red Soil exploitation
红壤垦殖
4) latosolic red soil
赤红壤
1.
Effect of medium and micro elements fertilizers on the yield and sugar of sugarcane in latosolic red soil;
赤红壤施用中、微量元素肥料对甘蔗产量与糖分的影响
2.
Leaching characteristics of nitrogen and phosphorus in inorganic compound fertilizer from latosolic red soil in South China.;
华南赤红壤无机复合肥氮磷淋失特征
3.
A soil column method was applied to study influences of simulated acid rain on leaching characteristics of nitrogen and phosphorus from organic compound fertilizer in latosolic red soil in south China.
通过土柱模拟淋洗试验,研究了施用等量有机复合肥条件下,不同酸度模拟酸雨对赤红壤氮磷淋失特征的影响。
5) Lateritic Red Soil
赤红壤
1.
The Effect of Simulated Acid Rain on Weathering Process of Lateritic Red Soil in Heshan,Guangdong Province;
模拟酸雨对鹤山赤红壤风化过程的影响
2.
Effects of Soil and Water Loss on Lateritic Red Soil Major Microbial Physiological Function Groups
水土流失对赤红壤微生物主要生理功能类群的影响
3.
The effects of single and compound cations of Ca2+, K+ and Zn2+ on adsorption of cadmium (Cd) in lateritic red soil was measured by batch experiment.
采用等温平衡法,测定了钙、钾、锌单一或两两共存下赤红壤镉的吸附量,并应用Freundlich方程log[Cs]=logKf+nlog[Ce]分析了土壤镉的吸附特征。
6) latosol red soil
赤红壤
1.
Pot experiment was carried out to study the effects of PAA on fertilizer and water conservation of soil, using dry land latosol red soil and Chinese cabbage (Brassica chinensis L) as the tested soil and crop, irrigating with water and 0.
在旱地赤红壤上以小白菜(Brassica chinensis L。
2.
The pot and field experiments were carried out, using cabbage and capsium as tested crops respectively, to study the effect of high water absorbent resin(HWAR) and its fertilizer products on fertilizer and water conservation in latosol red soil and latosol.
在旱地赤红壤和砖红壤上分别以小白菜和辣椒为供试作物,进行盆栽试验和大田试验,以研究高吸水性树脂及其肥料制品对土壤水肥的保持作用。
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。
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参考词条