坦桑尼亚选定水稻灌溉方案的土壤特征和土壤肥力评价

IF 2.1 Q3 SOIL SCIENCE Frontiers in soil science Pub Date : 2023-05-24 DOI:10.3389/fsoil.2023.1171849
Said H. Marzouk, H. Tindwa, B. Massawe, N. Amuri, J. Semoka
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引用次数: 0

摘要

水稻(Oryza sativa L.)是坦桑尼亚种植的第二大谷类粮食作物,仅次于玉米(Zea mays L.),约占农业用地的18%。精耕细作导致土壤退化,有机质投入不足,养分失衡,导致水稻产量下降。本研究对坦桑尼亚莫罗戈罗地区两种水稻灌溉方案的土壤肥力状况进行了表征、分类和评估。通过这项研究获得的数据将对土地利用规划作出重大贡献,并将促进具有类似生态条件的地区的农业技术转让和其他发展。在Mkula和Mkindo灌溉方案下,所研究的土壤分别命名为MKU-P1和MKD-P1。共收集7个复合土壤样品(0 ~ 20 cm)进行土壤肥力评价。根据美国农业部(USDA)土壤分类系统和世界参考基地(WRB)土壤分类系统,利用地形、土壤形态特征、母质、自然植被、排水、侵蚀和实验室数据对土壤进行了分类。结果表明:土壤表层为砂质粘土壤土,底土为砂质粘土对粘土;土壤反应范围从中酸性(pH 5.7)到强碱性(pH 8.6)。研究区表层土壤和底土养分(速效钾+、全氮、土壤有机质和有机碳)均较低。根据美国农业部土壤分类,MKU-P1被归类为ineptisols cumulic humaquepts, MKD-P1被归类为veridsols fluvaquic,分别对应于WRB中的水下河流(loic, oxyaquic)和非农业河流(gleyic)。结果表明,这些水稻适于种植。然而,土壤的化学肥力被列为低肥力,与全氮缺乏有关;含有过量的铁和锰的磷、钾和钙;并且可能对作物造成毒性。因此,在建议的氮磷施用速率和施用时间内施用有机和矿物改良剂对于增加这些土壤的养分含量和尽量减少损失至关重要。MKD-P1地下地层的盐度需要进一步考虑。
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Pedological characterization and soil fertility assessment of the selected rice irrigation schemes, Tanzania
Rice (Oryza sativa L.) is the second cereal food crop grown in Tanzania after maize (Zea mays L.) and covers approximately 18% of the agricultural land. Soil degradation due to intensive cultivation along with low organic matter input and nutrient imbalance has led to a decline in rice crop yields. This study was conducted to characterize, classify, and assess the fertility status of soils in two rice irrigation schemes of Morogoro region in Tanzania. The data obtained through this study will contribute significantly to land use planning and will facilitate the transfer of agro-technology and other development of the regions with similar ecological conditions. The studied pedons were named MKU-P1 and MKD-P1 for Mkula and Mkindo irrigation schemes, respectively. A total of seven composite soil samples (0–20 cm) were collected for soil fertility assessments. Landform, soil morphological features, parent material, natural vegetation, drainage, erosion, and laboratory data were used to classify the soils in their respective order as per the United States Department of Agriculture (USDA) Soil Taxonomy and the World Reference Base (WRB) soil classification systems. Results showed that the pedons were sandy clay loam in the topsoil and sandy clay to clay in the subsoil; soil reaction ranged from medium acid (pH 5.7) to strongly alkaline (pH 8.6). The topsoil and subsoil nutrients of the studied pedons including available K+, total N, soil organic matter, and organic carbon are low. Based on the USDA Soil Taxonomy, MKU-P1 is classified as Inceptisols cumulic humaquepts and MKD-P1 as Vertisols Fluvaquentic endoaquerts corresponding to Subaquatic fluvisols (loamic, oxyaquic) and Irragric vertisols (gleyic) in the WRB, respectively. The pedons were ranked as suitable for rice production. However, the chemical fertility of the soil is ranked as low fertile associated with deficient in total N; available P, K+, and Ca2+ with excessive iron and manganese; and likely to pose toxicity to crops. The application of organic and mineral amendments in recommended rates and timing for N and P is therefore essential to increase the nutrient content of these soils and minimize losses. Salinity in the subsurface pedon MKD-P1 needs to be taken into future consideration.
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