SOIL OF PAMETIKARATA, EAST SUMBA: ITS SUITABILITY AND CONSTRAINTS FOR FOOD CROP DEVELOPMENT

Q4 Agricultural and Biological Sciences
B. Prasetyo, H. Sosiawan, S. Ritung
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引用次数: 1

Abstract

Pametikarata, Lewa subdistrict, is the priority area for food crop development in East Sumba. To evaluate its suitability and constraints, chemical properties, suitability and fertility capability classification for rice and secondary crops of some potential soils have been studied both in the field and in the laboratory. Seven soil profiles consisted of forty one soil samples were subjected to chemical and mineralogical analyses in the laboratory. The analyses consisted of clay fraction and organic-carbon contents, pH, potential P and K (25% HCI extraction), available P, phosphate retention. Exchangeable cations and cation exchange capacity (NH4OAc 1N, pH 7), and mineralogical composition of the clay fraction. The results indicate that soil acidity varies from acid to neutral Exchangeable cations are dominated by Ca cation and soil CEC ranges from low to very high. Clay mineral composition also varies, some are dominated by montmorillonite, others show mixed mineralogy between montmorillonite and kaolinite, and the rests are dominated by kaolinite with the exception of wet Vertisols, all soils are grouped as marginally suitable (S3) for rice and secondary crops. Nutrient availability and retention are the common limiting factors. Using fertility capability classification (FCC), all soils are grouped as clayey soils with low infiltration and high water holding capacity. The serious constraint for food crop development in this area is uncontrolled grazing that makes a conflict of interests between farming and cattle herding systems. Optimum success of food crop development in the area could be reached by controlling the herding system and improving the existing agricultural system.
东松巴帕梅提卡拉塔土壤:对粮食作物发展的适宜性和制约因素
勒瓦区Pametikarata是东萨姆巴粮食作物开发的优先地区。为了评价其适宜性和限制条件,在田间和实验室对一些潜在土壤的化学性质、对水稻和次生作物的适宜性和肥力分类进行了研究。由四十一个土壤样本组成的七个土壤剖面在实验室中进行了化学和矿物学分析。分析包括粘土组分和有机碳含量、pH、电位P和K(25%HCI提取)、有效P和磷酸盐保留率。可交换阳离子和阳离子交换容量(NH4OAc 1N,pH 7),以及粘土部分的矿物学组成。结果表明,土壤酸度从酸性到中性不等。可交换阳离子以Ca阳离子为主,土壤CEC从低到极高。粘土矿物成分也各不相同,一些以蒙脱石为主,另一些表现出蒙脱石和高岭石之间的混合矿物学,其余的以高岭石为主,除了湿的Vertisol,所有土壤都被归类为勉强适合水稻和次生作物的土壤(S3)。养分的可利用性和滞留性是常见的限制因素。使用肥力能力分类(FCC),所有土壤都被归类为低渗透和高持水能力的粘性土。该地区粮食作物发展的严重制约因素是不受控制的放牧,这导致农业和畜牧系统之间的利益冲突。该地区粮食作物发展的最佳成功可以通过控制放牧系统和改善现有农业系统来实现。
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来源期刊
Indonesian Journal of Agricultural Science
Indonesian Journal of Agricultural Science Agricultural and Biological Sciences-Soil Science
CiteScore
1.00
自引率
0.00%
发文量
5
审稿时长
12 weeks
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