摘要
研究表明,不同质地的土壤,施钾后钾的分布规律不一样,土壤保持钾的能力,在低施钾时〔<600mg/kg(以每公斤土含K2O量表示,下同)〕,容量因素(△Q)是:△Q壤>△Q粘>△Q砂,中量施钾时(600~800mg/kg),△Q壤=△Q粘>△Q砂,在高施钾时(>800mg/kg),△Q粘>△Q壤>△Q砂。钾缓冲因素变化规律与容量因素一致。施钾在土壤液相和固相的分布规律符合Y=C-abx方程。建议一次施钾量的最佳点应是△B≈2.0,砂、壤、粘分别为150。
The potassium instantaneous potential buffer characteristics is vary in different texture soils.The capability of the soil keeping potassium,the capacity factor (△Q) is: △Q loam >△Q clay >△Q sand under lower level of K 2O application (<600 mg·kg -1 ),△Q loam =△Q clay >△Q sand under middle level of K 2O application (600~800 mg·kg -1 ), △Q clay >△Q loam >△Q sand under higher level of K 2O application (>800 mg·kg -1 ).The change laws of the buffer of the potassium are the same as the capacity factor.After applying K 2O,the law of potassium distributing in the liquid phase and solid phase of different texture soils accords with equation Y=C-ab x . It is suggested that the best amounts of potassium application once should be △B≈2.0, the sandy soil loamy soil and clayey soil should be 150,390 and 360 mg·kg -1 resp.
出处
《河南农业科学》
CSCD
北大核心
1996年第11期21-24,共4页
Journal of Henan Agricultural Sciences