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Topographic distribution of the soil total carbon content and sulfur deficiency for rice cultivation in a floodplain ecosystem of the Northern region of Ghana. (Special Issue: Crop resilience.)

机译:加纳北部洪泛区生态系统中水稻种植的土壤总碳含量和硫缺乏的地形分布。 (特刊:作物抗逆力。)

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An understanding of the spatial variation in soil fertility is fundamental for extending rice cultivation and developing appropriate management practices in currently under-utilized floodplain ecosystem of West Africa. The spatial patterns in the soil total carbon (TC) contents were analyzed using a Quickbird imagery, a global digital elevation model (ASTER-GDEM) and ArcView GIS functions for a White Volta floodplain of northern Ghana. An irrigated pot experiment was then conducted to relate rice biomass production to the spatial TC distribution and to identify deficient nutrients using different fertilizer treatments. The TC contents showed great variability (2.0-40.2 g kg-1) in a lognormal distribution, and the values were logarithmically increased with the proximity to reservoirs, consisting of a main river, back-swamps and ponds. The spatial pattern in the TC contents corresponded to the length of the waterlogging period during the rainy season, which was also logarithmically increased with the proximity to reservoirs, as estimated from the time-series satellite images. The corresponding patterns indicated that the spatio-temporal hydrological variable was a principal factor for the variance in the soil TC contents. Regarding the pot experiment, the amounts of soil mineralizable nitrogen were in accordance with the TC contents and correlated linearly with the plant N uptakes. However, dry matter production was scarcely relevant to the N-supplying capacity of the soils. Limited S concentrations in the plant tissues and a significant response to S application indicated that an inherent S deficiency restricted the dry matter production. NPK application without S increased only the N concentration and N:S concentration ratio in the plant tissues but not the biomass production. The high N-supplying capacity of the soil was related to the seasonal flooding, and the productive land areas for rice cultivation in both indigenous N and water availability were quantitatively predicted as a logarithmic function of the distance to reservoirs. Appropriate S supplementation would be required to utilize effectively the local N supply for rice biomass production in this under-utilized floodplain ecosystem.
机译:了解土壤肥力的空间变化,对于在目前尚未充分利用的西非洪泛区生态系统中扩大水稻种植和发展适当的管理做法至关重要。使用Quickbird影像,全球数字高程模型(ASTER-GDEM)和ArcView GIS功能对加纳北部的白色沃尔特洪泛区进行了土壤总碳(TC)含量的空间格局分析。然后进行了灌溉盆栽试验,以将水稻生物量生产与空间TC分布相关联,并使用不同的肥料处理方法来识别营养不足。 TC含量显示出对数正态分布的极大变化(2.0-40.2 g kg -1 ),并且值随着对水库(主要河流,回沼泽和池塘)的临近而对数增加。 。 TC含量中的空间模式对应于雨季的涝期长度,根据时间序列卫星图像估计,其随着对储层的接近也呈对数增加。相应的模式表明,时空水文变量是土壤TC含量变化的主要因素。关于盆栽试验,土壤可矿化氮的含量与TC含量一致,并与植物氮素吸收呈线性关系。但是,干物质生产与土壤的氮供应能力几乎无关。植物组织中有限的S浓度和对S施用的显着响应表明,固有的S缺乏限制了干物质的生产。在不添加S的情况下施用NPK只会增加植物组织中的N浓度和N:S浓度比,而不会增加生物量的产生。土壤的高氮供应能力与季节性洪水有关,并且定量预测了稻田中本地氮和水可利用量的稻田生产面积是距水库距离的对数函数。在未充分利用的洪泛区生态系统中,需要适当补充硫以有效利用当地氮素供应水稻生物量生产。

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