黄土高原坡地苹果园土壤肥力及矿质氮累积分析
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2009
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Resumo |
采用田间取样与室内分析相结合的方法,研究了黄土高原坡地苹果园肥力状况与矿质氮累积。结果表明,坡地苹果园土壤肥力低,氮、磷严重缺乏,钾相对丰富,土壤属于砂壤土,通气性强,保肥、保水性差。0—60cm土层土壤有机质含量为9.24~28.12g/kg,全氮为0.22~0.60g/kg,速效磷为0.17~16.08mg/kg,速效钾为80.06~168.39mg/kg;黄土高原坡地苹果园中NO3-—N有深层累积分布,累积深度大于2m,在180—200cm层最高累积量达249.61kg/hm2,而NH4+—N无深层累积。不同施肥处理对土壤剖面中的NH4+—N和NO3-—N含量分布影响不同,对NH4+—N含量和分布影响不明显,但不同施肥方式对NO3-—N含量分布影响显著。施加氮肥促进NO3-—N深层累积,施加磷肥有助于降低土层中的NO3-—N含量,缩小富集量的分布范围。 Soil fertility and mineral N accumulation of slope apple orchard on the Loess Plateau are studied. Results show that soil appears low-fertility due to the serious lack of N and P. Soil is sandy loam, with better soil aeration and poor water and nutrient retention. Fertility status of slope apple orchard on the Loess Plateau is low on the whole. The content of soil nutrients of the 0—60 cm soil layer is as follows: organic matter is 9.24~28.12 g/kg; total N is 0.22~0.60 g/kg; available P is 0.17~16.08 mg/kg;... |
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Idioma(s) |
中文 |
Fonte |
闫亚丹, 徐福利, 邹诚, 万超.黄土高原坡地苹果园土壤肥力及矿质氮累积分析.水土保持通报,2009,4: |
Palavras-Chave | #坡地 #苹果园 #黄土高原 #矿质氮 |
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期刊论文 |