孟加拉国不利生态系统中集约稻作系统下土壤植物养分状况

P. Saha, S. Islam, M. Islam, J. Biswas, M. Haque
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引用次数: 8

摘要

土壤肥力和作物产量因生态因子和土壤母质而异。对孟加拉国不同农业生态区(AEZ -18)不利生态系统土壤养分状况进行了基线研究。潜水和寒冷,AEZ-3;潮汐洪水生态系统,AEZ-13;干旱和寒冷易发地区,AEZ-26和haor地区,AEZ-21)。在0 ~ 20 cm深度共采集125个复合土壤样品(10样/点),保留了村庄、联盟、村、土地类型、土壤系列和土地利用模式的地理位置和数据。分析土壤样品的质地、pH、电导率(EC)、有机质(OM)、全氮(N)、有效磷(P)、交换性钾(K)、钙(Ca)、镁(Mg)、有效硫(S)和锌(Zn)。AEZ-18、aez - 3和aez - 13土壤pH呈微酸性至中性。AEZ-21土壤呈强酸性,AEZ-26土壤呈中性至微碱性。在大多数地点,80% ~ 96%的土壤有机质低于临界水平(1.72%)。除AEZ-21外,其余土壤氮含量均低于临界水平(0.12%)。在AEZ-21中,100%的样品缺磷,在AEZ-26中缺磷的比例为24%。在AEZ-3中,60%的样品缺钾,在AEZ-26中,这一比例为40%。AEZ-3缺S的样品分别为32%和24%,缺S的样品为26%。在AEZ-18中缺锌最多(84%),其次是AEZ-21(48%)。AEZ-3缺钙约占52%,其次是AEZ-21(4%)。土壤养分状况普遍较低,且各地区差异较大。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
SOIL PLANT NUTRIENT STATUS UNDER INTENSIVE RICE-FARMING SYSTEMS IN UNFAVORABLE ECO-SYSTEMS OF BANGLADESH
Soil fertility and crop production varies depending on ecological factors and soil parent materials. A baseline study was conducted to delineate soil nutrient status of unfavorable ecosystems under different agro-ecological zones (AEZ) of Bangladesh (Char and saline, AEZ-18; submergence and cold, AEZ-3; tidal flood ecosystem, AEZ-13; drought and cold prone, AEZ-26 and haor area, AEZ-21). A total of 125 composite soil samples (10 samples/spot) were collected at 0-20 cm depth, maintained geographical positions and data on village, union, upazila, land type, soil series and land use patterns. Soil samples were analyzed for texture, pH, electrical conductivity (EC), organic matter (OM), total nitrogen (N), available phosphorus (P), exchangeable potassium (K), calcium (Ca), magnesium (Mg), available sulfur (S) and zinc (Zn). Soil pH was slightly acidic to neutral in AEZ-18, 3 and 13. In AEZ-21, soil was strongly acidic but neutral to slightly alkaline AEZ-26. In most locations, soil OM was below critical level (1.72%) in 80 to 96% samples. Soil N was below critical level (0.12%) in almost all samples except in AEZ-21. In AEZ-21, 100% samples showed P deficiency and in AEZ-26 it was 24%. In AEZ-3, 60% samples were K deficient and in AEZ-26 it was 40%. Thirty-two and 24% samples were S deficient in AEZ-3 and 26, respectively. The highest 84% samples were Zn deficient in AEZ-18 followed by AEZ-21 (48%). About 52% samples were Ca deficient in AEZ-3 followed by AEZ-21 (4%).  Nutrient status of soils was mostly low and varied among locations.
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