1) flow aquic paddy soil
潮土性水稻土
2) acid paddy soil
酸性水稻土
1.
Study on uptake of Si, K, Ca, Mg by rice and its dynamics in acid paddy soil;
酸性水稻土上水稻对硅、钾、钙、镁的吸收及其动力学研究
3) Purple Paddy Soil
紫色土性水稻土
1.
Distribution of Organic Carbon in Purple Paddy Soils;
紫色土性水稻土有机碳分布特征
4) Percogenic paddy soils
渗育性水稻土
5) red paddy soil
红壤性水稻土
1.
Effects of long-term different fertilization on labile organic carbon in red paddy soil;
长期施肥对红壤性水稻土活性碳的影响
2.
A 24-year field experiment was conducted to study the effects of long-term fertilization on the soil organic carbon(SOC) and total nitrogen (TN) contents in various horizons of red paddy soil in Jinxian County of Jiangxi Province(116°20′24″N,28°15′30″E).
在实施24 a的长期田间定位试验区,研究了不同施肥处理对红壤性水稻土剖面有机碳及全氮含量的影响。
3.
One of the aims of the experiment was to study soil organic carbon (SOC) distribution and storage in different size groups of micro-aggregate in surface layer (0-17cm) of red paddy soil impacted by different fertilizers.
在田间定位试验区 ,研究了不同施肥处理对表层红壤性水稻土微团聚体组成以及土壤有机碳在各级微团聚体中分布和赋存的影响。
6) paddy soil derived from red earth
红壤性水稻土
1.
Effects of long-term fertilization on soil organic nitrogen components in paddy soil derived from red earth;
长期施肥对红壤性水稻土有机氮组分的影响
2.
：Based on the long-term fertilizer experiment（19 years）in paddy soil derived from red earth, the methods proposed by Jiang & Gu（1989）are adopted to study the effects of long-term fertilization on the accumulation and loss of the soil phosphorus and on the forms of soil inorganic phosphorus in paddy soil.
通过红壤性水稻土19 a肥料长期定位试验，结果表明，不施磷处理的土壤磷素处于耗竭状态，耕层土壤全磷含量持续下降，但耕层以下土层的全磷尚未耗损；连年施磷的土壤耕层全磷含量提高，提高的幅度呈现明显量级关系。
3.
The rules of Mn uptake by early and late rices at different growth stages in the paddy soil derived from red earth were studied based on the long-term stationary experiment of Hunan Agriculture University.
以湖南农业大学1982年布置的长期定位实验为依托,研究了红壤性水稻土早、晚稻吸锰规律。
补充资料：水稻土
| 水稻土 paday soil 长期种植水稻形成的具有氧化还原交替特点的耕作土壤。长期植稻引起土壤有机质含量增加，有机质组成趋于简单；饱和土壤中盐基淋溶，不饱和土壤发生复盐基作用；铁、锰元素在土壤中移动，耕层含量较低，淀积层较高，潜育层最低；粘粒矿物发生分解和合成。随着水稻土形成作用的发展，出现水稻土特有的发生层：耕作层、犁底层、淀积或斑纹层、漂洗层、潜育层。水稻土分布极广，凡气候适宜又有水源灌溉的土壤均可经种植水稻而形成。主要分布在北纬35°至南纬23°之间，以亚洲最多。中国集中在长江下游平原、四川盆地、珠江三角洲和台湾西部平原。水稻土的类型主要有：①淹育性水稻土。多分布在丘陵，地下水位低，耕层浅，肥力不高。②潴育性水稻土。分布于冲积平原，地下水位一般60～150厘米，土壤通透性好，矿质养分丰富，肥力高。③潜育性水稻土。分布在丘陵谷地或冲积平原洼地，土质轻粘，有的有泥核，耕作困难，有效养分低，尤磷、钾不足。④漂洗型水稻土。在下降水或侧渗水影响下形成，土层紧实，通透性差，有机质含量低，养分贫乏。高产水稻土应是耕层深厚，犁底层不太紧实，通气透水，质地适中，耕性良好，水渗透快慢适度，养分供应协调。
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