1) Sinnamon and fluvo-aquic soils
褐土潮土
2) fluvo-aquic soil
褐潮土
1.
Effect of long-term fertilization on accumulation, transformation and availability of phosphorus in Fluvo-aquic soil;
长期施肥对褐潮土磷素积累、形态转化及其有效性的影响
3) cinnamon soil
潮褐土
1.
communis tsen et Lee] with full intersectant design in cinnamon soil.
采用盆栽的试验方法,运用正交设计,研究了潮褐土区域土壤重金属Cd、Zn复合污染对小白菜生长的影响。
2.
Successive extraction method was adopted to study the relationship between characteristics of chemical forms of cadmium and lead and four soil enzymatic activities (calatase, urease, invertase, alkalin phosphatase) in alluvial meadow soil and meadow cinnamon soil in the plain of Hebei by pot experiment .
采用网室盆栽试验 ,运用连续提取方法 ,研究了河北平原潮土、潮褐土 2种土类上Cd、Pb的化学形态特征与 4种土壤酶活性 (脲酶、H2 O2 酶、转化酶、碱性磷酸酶 )间的关系。
4) meadow cinnamon soil
潮褐土
1.
The effect of different nitrogen application on meadow cinnamon soil CO2 emission of winter wheat in North China Plain was further discussed.
)返青期、拔节期、孕穗期、灌浆期和成熟期进行了土壤呼吸速率的测定,探讨了不同氮肥用量对华北平原潮褐土区冬小麦农田土壤CO2释放的影响。
2.
Eight years location experiment was conducted in meadow cinnamon soil in Hebei Province to study the effect of returning straw into field on characteristics of absorbed and desorbed P in soil and micro-aggregates,the changes of P absorption and desorption capacity under different fertilizer regimes from the view points of the storage of P in various micro-aggregates.
通过8年定位试验,研究了秸秆还田对潮褐土及其微团聚体磷素吸附与解吸特性的影响,从各级微团聚体磷素吸附与解吸储量角度探讨了不同施肥制度下土壤磷素吸附与解吸性能的变化实质。
3.
Incubation and micro field plot experiment were carried out to study the transformation and its influence factors of applied P in the meadow cinnamon soil in Hebei province.
利用培养及微区试验 ,研究磷肥施入潮褐土后的动态转化及其影响因素。
5) Cinnamon soil
褐土
1.
Effect of P and Cd interaction on bioavailability of P and Cd in Cinnamon soil;
褐土中磷镉交互作用对磷镉有效性影响
2.
Effects of long-term inorganic fertilizer combined with organic manure on microbial biomass C、N and enzyme activity in cinnamon soil;
长期有机无机肥配施对褐土微生物生物量碳、氮及酶活性的影响
3.
Effect of nitrogen and potassium ratio on chemical components in tobacco leaves grown in cinnamon soil;
褐土上不同氮、钾比例对烟叶化学成分的影响
补充资料:潮土
潮土 chao soil 河流沉积物受地下水运动和耕作活动影响而形成的土壤。因有夜潮现象而得名。其主要特征是地势平坦、土层深厚。集中分布于河流冲积平原、三角洲泛滥地和低阶地。中国潮土多分布于黄河中、下游冲积平原及其以南江苏、安徽的平原地区和长江流域中、下游的河、湖平原和三角洲地区。潮土的形成主要受河流沉积物、地下水和耕作的影响。中国的潮土分2个亚类:黄潮土,以黄河沉积物为主,土壤中的碳酸钙及可溶性盐含量略偏高,呈中性至碱性反应,有机质含量不高;灰潮土,成土物质主要为硅铝质风化物,大多不含石灰,呈中性至微酸性反应,土壤毛管作用强,透水性较好,生物活动层深厚,土壤较肥沃。潮土的性状良好,适种性广,其分布地区是中国的粮棉基地。 |
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