1) purple stagnic anthrosols
紫色水耕人为土
2) Stagnic anthrosols
水耕人为土
1.
Electrical conductivity and fertility evaluation of stagnic anthrosols in the typical region of upper reaches of the Yangtze river;
长江上游典型区水耕人为土的电导率与肥力评价探讨
2.
Features of Microstructure of Diagnostic Horizons and Lower Categorical Classification of Stagnic Anthrosols in Chengdu Plain;
成都平原水耕人为土诊断层的微形态特征与土壤基层分类
3.
Soil Properties and SEM Features of Diagnostic Horizon of Stagnic Anthrosols in Southwestern,China
西南地区水耕人为土诊断层土壤特性及SEM特征
3) hydragric anthrosols
水耕人为土
1.
Soil Classification of Main Hydragric Anthrosols in the Chengdu Plain;
成都平原主要水耕人为土土系的划分研究
2.
A detailed description is given in this paper of the selection process for classification factors on soil series of hydragric anthrosols (or paddy soils), with 10 typical soil samples on Chengdu Plain as case study, based on the summing-up of the relevant selection principles and bases.
在总结水耕人为土土系划分指标选取原则及依据的基础上,以成都平原10个典型土样为例,详细阐述了指标选取过程。
3.
The micro-tructure of several typical redoxi-orphic features of Hydragric Anthrosols were analyzed by combining micro-orphological observation and Electronic Energy Disperse Spectrometer (EDS) determination of micro-one chemical composition.
结合微形态观察和特征微区化学成分的电子能谱测定，对水耕人为土几种典型的氧化还原形态特征的结构进行了解析，并在此基础上提出了它们的形成机理。
4) ancient stagnic anthrosols
古水耕人为土
1.
The typical ancient stagnic anthrosols of Sanxingdui site had been selected to probe the diagnostic horizons characteristics and forming processes, results showed that the ancient stagnic anthrosols which were formed in long time and high developmental degree had the characteristics of obviously horizons differentiation.
选定广汉三星堆遗址的典型古水耕人为土,研究剖面的诊断层特性与形成过程,取得了以下主要研究结果:形成时期长、发育程度高的古水耕人为土,在土壤剖面形态和特性上,表现出明显的层次分化。
5) no-tillage purple paddy soil
免耕紫色土水稻田土壤
6) slope cropland in purple soil
紫色土坡耕地
1.
A field experiment was carried out in hilly area of central Sichuan Basin to study the characteristics of phosphorus loss by runoff from slope cropland in purple soil.
通过对川中丘陵不同施肥试验田径流、泥沙和磷素流失的观测与测定分析,研究了暴雨下平衡施肥对紫色土坡耕地水土流失与土壤磷素随径流流失的特征。
补充资料：紫色土
| 紫色土 purplish soil 发育于亚热带地区石灰性紫色砂页岩母质土壤。全剖面呈均一的紫色或紫红色，层次不明显。主要分布在中国的亚热带地区，以四川盆地为主。紫色土是在频繁的风化作用和侵蚀作用下形成的，其过程特点是：物理风化强烈、化学风化微弱、石灰开始淋溶。紫色土土层浅薄，通常不到50厘米，超过1米者甚少。一般含碳酸钙，呈中性或微碱性反应。有机质含量低，磷、钾丰富。由于紫色土母岩松疏，易于崩解，矿质养分含量丰富，肥力较高，是中国南方重要旱作土壤之一，除丘陵顶部或陡坡岩坎外，均已开垦种植。因侵蚀和干旱缺水现象时有发生，利用时需修建梯田和蓄水池，开发灌溉水源。开辟肥源以增加土壤有机质和氮的含量，也是提高其生产力的重要措施。
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参考词条