帕米桑区水稻保留评估

Khofifah Nur Syamsiyah, K. Wicaksono
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引用次数: 1

摘要

2011年至2019年,帕梅卡桑县的水稻产量下降了38.71%,原因是农民施用的肥料与植物需求不匹配,例如粪肥、有机肥和其他无机肥料的施用不足。此外,农民获得的基本肥料来自非正式信息,因此在土地上施用肥料效率不高。为了克服这些问题,人们从养分保持方面评价土壤肥力,作为确定肥料需要量的基础。本研究的目的是从土壤肥力的角度,特别是从水田养分保持的角度来评价帕梅卡桑县的土壤肥力。本研究采用基于SPL (Land Map Unit)的有目的随机抽样方法。观察的参数包括阳离子交换容量、有机碳、碱饱和度、pH、电导率、织构、孔隙率、容重和饱和水力导率。结果表明:帕梅卡山县土壤肥力水平较高,其中阳离子交换容量为43.92 cmol kg-1,碱基饱和度为99.38%,pH值为7.00,电导率为0.39 mS,主要质地为粘土组分。Waru和Kadur地区土壤有机碳肥力水平低(0.08%),pasan地区土壤容重低(1.59 g cm-3), Proppo地区土壤孔隙度低(34.89%),pasan地区土壤饱和导水率低(46.34 cm h -1)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
EVALUASI RETENSI HARA PADA LAHAN PADI DI KABUPATEN PAMEKASAN
Rice production in Pamekasan Regency from 2011 to 2019 decreased by 38.71% due to farmers applying fertilizers that did not match plant needs, such as insufficient application of manure, organic fertilizers and other inorganic fertilizers. In addition, the basic fertilization obtained by farmers comes from informal information, so the application of fertilizers on the land is not efficient. Efforts have been made to overcome these problems by evaluating soil fertility from the aspect of nutrient retention as a basis for determining fertilizer requirements. The purpose of this study was to evaluate soil fertility, especially from the aspect of nutrient retention in paddy fields in Pamekasan Regency. This research used a purposive random sampling method based on SPL (Land Map Unit). Parameters observed were cation exchange capacity, organic C, base saturation, pH, electrical conductivity, texture, porosity, bulk density and saturated hydraulic conductivity. The results showed that the high level of soil fertility in Pamekasan Regency was found in cation exchange capacity in Tlanakan District (43.92 cmol kg-1), base saturation in Galis District (99.38%), pH in Tlanakan District (7.00), electrical conductivity in Pakong and Pasean districts (0.39 mS) and the dominant texture is the clay fraction. Low fertility levels are found in soil organic C in Waru and Kadur Districts (0.08%), bulk density in Pasean District (1.59 g cm-3), porosity in Proppo District (34.89%), and saturated hydraulic conductivity in Pasean District (46.34 cm hour-1).
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