Temporal variation in the soil properties and rice yield of organic rice farming in the tropical monsoon region, Indonesia

J. Syamsiyah, D. Ariyanto, K. Komariah, A. Herawati, Pertiwi Kurnia Dwisetio, Safira Indrias Sari, Harjayanti Auliyaa Salsabila, Ganjar Herdiansyah, S. Hartati, M. Mujiyo
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Abstract

One of the organic farming goals is improving soil properties to support sustainable rice production. This study investigated the soil properties and rice yields under temporal variation of organic rice fields. Soil sampling was conducted in organic rice fields with three temporal variations, namely 0, 4, 7, and 10 years in a tropical monsoon region in Central Java, Indonesia. Variables observed included soil organic carbon, soil carbon stock, soil microbes population, dissolved organic carbon, soil liquid limit, soil sticky limit, soil plasticity limit, soil color changing limit, soil friability, soil porosity, soil total nitrogen, soil total phosphorus, soil available sulfur, exchangeable calcium, cation exchange capacity, total potassium, bulk density, base saturation, exchangeable sodium, exchangeable potassium, and rice yield.  This study confirms that soil organic carbon increased by 51.63% within 10 years (from 1.84% to 2.79%). Organic farming also improved all the physical, chemical, and biological soil properties, by the increase of soil organic carbon. However, soil organic carbon is mostly determined by soil cation exchange capacity, soil total phosphorus, and soil porosity. The mechanism of rice yield increase in organic rice farming is not affected by soil organic carbon directly but through the synergic increase in soil total nitrogen. The 1% increase of soil organic carbon increases 0.065% of soil total nitrogen hence rice yield increases by 1.66 tons ha-1. This study supports sustainable agriculture by providing evidence of improved soil properties under organic farming.
印度尼西亚热带季风区有机水稻种植的土壤特性和水稻产量的时间变化
有机农业的目标之一是改善土壤特性,以支持可持续的水稻生产。本研究调查了有机稻田时间变化下的土壤特性和水稻产量。在印度尼西亚中爪哇热带季风区的有机稻田中进行了土壤取样,取样有三种时间变化,即 0 年、4 年、7 年和 10 年。观测变量包括土壤有机碳、土壤碳储量、土壤微生物数量、溶解有机碳、土壤液限、土壤粘限、土壤塑性限、土壤变色限、土壤易碎性、土壤孔隙度、土壤全氮、土壤全磷、土壤可利用硫、可交换钙、阳离子交换容量、全钾、容重、碱饱和度、可交换钠、可交换钾和水稻产量。 这项研究证实,土壤有机碳在 10 年内增加了 51.63%(从 1.84% 增加到 2.79%)。通过增加土壤有机碳,有机耕作还改善了土壤的物理、化学和生物特性。然而,土壤有机碳主要由土壤阳离子交换容量、土壤全磷和土壤孔隙度决定。有机水稻种植的水稻增产机理并不直接受土壤有机碳的影响,而是通过协同增加土壤全氮来实现的。土壤有机碳增加 1%,土壤全氮增加 0.065%,因此水稻产量增加 1.66 吨/公顷。这项研究为有机耕作下土壤性质的改善提供了证据,从而支持了可持续农业。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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