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1)  Soil dynamic submergence
土壤淹水变化
2)  waterlogged soil
淹水土壤
1.
Research progress of the forms and effectiveness of As in waterlogged soil;
淹水土壤中砷的形态及有效性研究进展
2.
Selenium transport in waterlogged soil was primarily controlled by reductive leaching of seleniun iron compounds,and next by fumaric selenium leaching as well as mechanical leaching(or clay leaching).
对模拟土柱淋溶下的 1 5~ 2 0 ,35~ 45 ,75~ 85 cm土层土壤作各种形态硒含量测定 ,结果表明 ,淹水土壤硒的迁移主要受硒铁化合物还原淋溶机制控制 ,其次受富里酸键合硒淋溶及机械 (粘粒 )淋溶等机制的影响 ;外加的叶蛋白硒在土壤中分解成水溶性有机硒随水淋溶 ,少量以富里酸硒积累在中下层土壤 。
3)  Flooded soil
淹水土壤
1.
Effects of straw incorporation on the solubility of cadmium and copper in flooded soil;
施用秸秆对淹水土壤镉、铜溶出的影响
2.
A recirculating flume simulated experiment was carried out to estimate phosphorus release properties and infection in different layers of flooded soils.
采用土槽模拟实验研究了淹水土壤不同土层磷释放特征及影响因素。
4)  submerged soil
淹水土壤
1.
N labelled rice straw and maize straw were used to study the transformation of 15 N in submerged soil by using 15 N tracer technique and sealed incubation method.
采用15N示踪技术和密闭培养法研究水稻和玉米秸秆15N在淹水土壤中的转化过程。
5)  flooded paddy soil
淹水稻田土壤
1.
Kinetics and mathematic simulation of nutrient release from coated controlled release fertilizer under the condition of flooded paddy soil;
淹水稻田土壤条件下包膜控释肥料养分释放的动力学与数学模拟
6)  submerged soil/rice straw
淹水土壤/秸杆
补充资料:土壤水分运动基本方程(见土壤水运动)


土壤水分运动基本方程(见土壤水运动)


turang shuifen yundong iiben土壤水分运动基本方程fangeheng见土壤水运动。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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