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Chemical fractionation of phosphorus in calcareous soils of Hamedan, western Iran under different land use

机译:不同土地利用方式下伊朗西部哈马丹钙质土壤中磷的化学分馏

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We investigated the effects of land uses on P distribution and availability in selected calcareous soils under different management practices. KCl-P (labile P), NaOH-P (Fe-Al-bound P), HCl-P (Ca-bound P), and residual P (Res-P) fractions at 0-30cm depth were determined for soils planted to garlic, orchard, pasture, potato, leafy vegetables, and wheat. Trends in P distribution between chemical fractions were similar between land uses. Ca-bound P was the most abundant P fraction in the soils, constituting between 61% and 78% of the total P, whereas P associated with labile was less abundant (< 2%). Soils under leafy vegetables and wheat along with pasture presented the highest and lowest values in all fractions of P, respectively. Labile P generally was highest for leafy vegetables and potato. Labile P and Fe-Al-bound P comprised < 1.4% and 8% of total P, respectively. Residual P ranged from ≈ 14% (potato and garlic) to 31% (pasture). Long-term fertilization increased P allocation to inorganic fractions, as Ca-bound P contained 78% of total P for potato and garlic and 74% for leafy vegetables but 61% for pasture. A strong positive correlation between labile P and Fe-Al-bound P (r = 0.534, p < 0.01), labile P and Ca-bound P (r = 0.574, p < 0.01), Ca-bound P and Fe-Al-bound P (r = 0.504, p < 0.01), Olsen-P and CaCl_2-P (r = 0.821, p < 0.01) was found. Principal-component analysis showed that the first four components accounted for most of the variation, 32.5%, 16.9%, 12.9%, and 7.9% of total variation, respectively.
机译:我们调查了在不同管理方式下,土地利用对选定钙质土壤中磷分布和有效性的影响。确定了在0-30cm深度下种植的土壤的KCl-P(不稳定P),NaOH-P(Fe-Al结合P),HCl-P(Ca结合P)和残留P(Res-P)级分。大蒜,果园,牧场,土豆,多叶蔬菜和小麦。不同土地用途之间化学成分之间的磷分布趋势相似。钙结合的磷是土壤中最丰富的磷组分,占总磷的61%至78%,而不稳定的磷含量较低(<2%)。叶面蔬菜和小麦下的土壤以及牧草在所有比例的磷中分别呈现最高值和最低值。叶菜类蔬菜和马铃薯的不稳定磷通常最高。不稳定的P和与Fe-Al结合的P分别占总P的<1.4%和8%。残留磷的范围从≈14%(马铃薯和大蒜)到31%(牧草)。长期施肥增加了磷向无机部分的分配,因为钙结合的磷占马铃薯和大蒜总磷的78%,叶类蔬菜占74%,牧场占61%。不稳定P和Fe-Al结合的P(r = 0.534,p <0.01),不稳定P和Ca结合P(r = 0.574,p <0.01),Ca结合P和Fe-Al-结合P(r = 0.504,p <0.01),Olsen-P和CaCl_2-P(r = 0.821,p <0.01)被发现。主成分分析表明,前四个成分占变异的大部分,分别占总变异的32.5%,16.9%,12.9%和7.9%。

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