2) fluvo-aquic soil
潮土
1.
Effect of long term fertilizers and organic inputs on balance and fate of nitrogen in fluvo-aquic soil;
长期施用有机和无机肥对潮土氮素平衡与去向的影响
2.
Effect of long-term fertilization on K~+ desorption kinetics of noncalcareous fluvo-aquic soil;
长期定位施肥对非石灰性潮土K~+解吸动力学的影响
3.
Study on relationship of soil nutrients and various particlesin fluvo-aquic soils on the Yellow River flood plain,north China;
华北黄泛平原潮土土壤养分与土壤粒级的关系研究
3) Alluvial soil
潮土
1.
Composing, transforming and supplying characters of inorganic phosphorus in north Heilonggang s alluvial soil;
黑龙港北部潮土无机磷组成转化及供磷特性研究
2.
A field plot experiment was conducted in Alluvial soil of Hebei plain and effects of five kinds of NP compound and combined fertilizers on yield of wheat and corn were studied.
在河北平原潮土区，就５种氮磷复（混）合肥料对小麦、玉米的增产效果进行了研究。
3.
The maximum amount of nutrients adsorbed, stable time to extract the nutrients needed in alluvial soil, the effect of soil moisture on nutrient extracted by resin membrane were studied using domestic and imported ion exchange resin membranes in room simulated condition.
本研究采用国产和进口的离子交换树脂膜，在室内模拟条件下研究了不同类型膜的饱和吸附量、在潮土养分测定的稳定提取时间、不同土壤含水量对潮土养分测定的影响等，结果表明：在1、2、5、8和12小时的吸附过程内，各种树脂膜对离子的吸附过程曲线均基本相同，但在吸附量上差异很大，若以单位面积的吸附量计算时，国产树脂膜的饱和吸附量均大于进口树脂膜；不同养分离子，进口树脂膜与国产树脂膜所吸附的养分离子数量比例也不相同，铵态氮的比例为1：2。
4) calcareous soil
潮土
1.
Effect of different nitrogen fertilizers on dynamic transformation of phosphorus fertilizer in calcareous soil;
不同氮肥对潮土中磷肥转化的动态影响
2.
The effects of different nitrogen fertilizers on the uptake of boron and molybdenum of rape in calcareous soil were inves- tigated in a pot experiment.
利用盆栽试验研究了潮土中不同氮肥对油菜硼钼吸收的影响,结果表明,前期(5周)施氮并没有促进油菜的生长,而且大部分氮肥对油菜生长表现抑制作用,氯化铵处理的作用最大,硫酸铵和尿素处理次之,硝酸铵处理再次之;不同氮肥均有抑制油菜生长前期(5周)硼吸收和累积的作用,其中以氯化铵、硝酸铵和尿素的作用为甚;不同氮肥同样抑制油菜生长前期(5周)对钼的吸收和累积,以硫酸铵处理作用最突出,氯化铵处理次之。
5) Chao soil
潮土
1.
Study on optional ratio of basic to dressing application of potassium fertilizer in high yield wheat field in Chao soil region;
潮土区高产麦田钾肥适宜基追比研究
2.
Effects of straw application with N , P fertilizer on available N and P contents in chao soil. Journal of Zhejiang Agricultural University, 1998,24(4):359～363;
秸秆配施氮磷化肥对潮土氮磷含量变化的影响
3.
Effect of Rare Earth Element Lanthanum on Microflora in Chao Soil;
稀土元素镧对潮土微生物区系的影响
6) Meadow soil
潮土
1.
Their impacts on sustainability indices of soil C and N showed the following order: organic integrated chemical fertilizer treatment > organic fertilizer treatment > chemical fertilizer treatement, and meadow soil > paddy soil > red soil.
结果表明，不同施肥方式、不同土壤类型对碳、氮养分可持续性指数的影响表现为有机肥配施化肥处理＞有机肥处理＞化肥处理，潮土＞水稻土＞红壤；对磷、钾养分表现为化肥处理＞有机肥配施化肥处理＞有机肥处理，水稻土＞潮土＞红壤。
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。 |
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