有机和常规蔬菜栽培体系下土壤磷在土壤中的吸附与释放

Aridinasty Maritasari, B. Purwanto, S. Utami
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引用次数: 0

摘要

磷(P)被土壤有机质和土壤无定形矿物等土壤组分强烈吸附,这些组分已被确定为影响土壤磷吸附和释放的因素。本研究的目的是表征印度尼西亚Merbabu山区有机和常规蔬菜种植系统中土壤磷的吸附和释放模式。从有机和传统农业系统的土层(0厘米至20厘米和20厘米至40厘米)中采集土壤样本。结果表明,有机农业系统在20~40cm深度的土壤中吸附率最高,在20~40km深度的低有机物输入的常规农业系统中吸附率最低,在低有机物投入的有机农业系统中磷的释放率也较高。结果表明,有机耕作体系中的蔬菜土壤不仅具有较高的吸磷能力,而且具有快速释磷的能力。
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Adsorption and release of soil P in andisols under organic and conventional vegetable farming system
Phosphorous (P) is strongly adsorbed by soil components, such as soil organic matter and soil amorphous minerals in Andisols, which have been identified as an influential factor in adsorption and release of soil P. The aim of this study was to characterize the pattern of soil P adsorption and release in both organic and conventional vegetable farming systems in Merbabu Mountain area, Indonesia. Soil samples were collected from soil layers (0 cm to 20 cm and 20 cm to 40 cm) in organic and conventional farming systems. The result showed that the highest adsorption rate was found in organic farming systems at a depth of 20 cm to 40 cm. The lowest adsorption rate was found in conventional farming systems with low input of organic matter at a depth of 20 cm to 40 cm. A higher rate of P release was also found in organic farming systems with a low input of organic matter. It can be concluded that vegetable soils in organic farming systems are not only highly capable of adsorbing P but also capable of releasing P rapidly.
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16
审稿时长
10 weeks
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