孟加拉Madhupur地区和北部及东部山前平原酸性土壤的理化性质

Asif Ahmed Ratul, T. Hoque, Rafiqul Islam, A. Hoque
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引用次数: 1

摘要

土壤反应是影响土壤肥力和作物生产力的重要问题。从Sherpur区nalbaria upazila的Ramchandrakura村、Bishgiripar村、Andharupara村和Nayabil村(AEZ 22- north and Eastern Piedmont Plains)和Mymensingh区Fulbaria upazila的Bakta村、Nishchintopur村、Boril村和Kaladaho村(AEZ 28-Madhupur Tract)的农民田间采集了25个具有代表性的土壤样品,研究了酸性土壤的理化性质。45份样品中,砂质壤土13份,粉质壤土17份,壤土10份,粘质壤土2份,壤土3份。土壤pH值呈极强酸性至强酸性。22区土壤pH值为3.81 ~ 4.78,28区土壤pH值为3.96 ~ 5.11。naliitabari土壤的有机碳含量在0.50 ~ 1.35%之间,Fulbaria土壤的有机碳含量在0.50 ~ 1.27%之间,处于中低水平。氮、磷、钾、硫等营养元素在大部分样品中处于极低或极低至中等水平。AEZ 22和AEZ 28的全氮含量分别在0.06 ~ 0.14%和0.07 ~ 0.16%之间变化。22区土壤有效磷含量在3.25 ~ 26.45 ppm之间,28区土壤有效磷含量在2.45 ~ 16.62 ppm之间。22区土壤的交换态钾变化范围为15.13 ~ 92.41 ppm, 28区土壤的交换态钾变化范围为16.09 ~ 98.41 ppm。AEZ 22土壤有效硫含量变化范围为1.68 ~ 33.70 ppm, AEZ 28土壤有效硫含量变化范围为3.95 ~ 27.52 ppm。因此,这些酸性土壤应施用石灰,并施用无机肥料和有机肥料,以保证作物的成功生产。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Physico-chemical properties of acid soils from Madhupur Tract and Northern & Eastern Piedmont Plains of Bangladesh
Soil reaction is an important issue that adversely affects soil fertility and crop productivity. Twenty five representative soil samples from farmers’ fields of Ramchandrakura, Bishgiripar, Andharupara and Nayabil villages of Nalitabari upazila under Sherpur district (AEZ 22-Northern and Eastern Piedmont Plains) and twenty soil samples from farmers’ fields of Bakta, Nishchintopur, Boril and Kaladaho villages of Fulbaria upazila under Mymensingh district (AEZ 28-Madhupur Tract) were collected and analyzed to study the physicochemical properties of acid soils. Among 45 samples, 13 were sandy loam, 17 were silt loam, 10 were loam, 2 were clay loam and 3 were loamy sand in texture. Soil pH was very strongly acidic to strongly acidic. The soil pH of AEZ 22 varied from 3.81 to 4.78 and that of AEZ 28 varied from 3.96 to 5.11. The organic C of Nalitabari soil varied from 0.50 to 1.35% and that of Fulbaria soils ranged from 0.50 to 1.27% showing low to medium status. The status of nutrient elements viz. N, P, K and S in most of the samples was very low or very low to medium. Total N contents of AEZ 22 varied from 0.06 to 0.14% and that of AEZ 28 varied from 0.07 to 0.16%. Available P in soils of AEZ 22 varied from 3.25 to 26.45 ppm and that in soils of AEZ 28 ranged from 2.45 to 16.62 ppm. Exchangeable K in AEZ 22 soils varied from 15.13 to 92.41 ppm and that in AEZ 28 soils varied from 16.09 to 98.41 ppm. Available S in AEZ 22 soils varied from 1.68 to 33.70 ppm and that in AEZ 28 soils from 3.95 to 27.52 ppm. Therefore, these acid soils should be amended with liming materials and fertilized with inorganic fertilizers and organic manures for successful crop production.
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