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Evaluation of soil physical quality of irrigated agroecosystems in a semi-arid region of North-eastern Brazil.

机译:巴西东北部半干旱地区灌溉农业生态系统土壤物理质量评估。

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Concern about soil physical quality has grown in recent years, particularly in view of serious problems caused by intensive soil use. We hypothesised that improper soil management in irrigated areas damages the structure of sensitive soils in some regions in North-eastern Brazil. The aim of the study was to evaluate the physical quality of irrigated soils planted with annual and perennial crops, compared with soils under natural vegetation in Ceara State, Brazil. Measurements were made of least limiting water range (LLWR), the S index, and relative density. Undisturbed soil samples were collected at two depths (5-10 and 20-25 cm) in four cultivated areas (banana, guava, pasture, and maize/bean in succession) and two natural vegetation areas (NV1, NV2) adjacent to the cultivated areas. All sites were in the Jaguaribe-Apodi Irrigated District, Limoeiro do Norte, Ceara, Brazil. The LLWR was determined using the water retention curve, soil resistance to penetration, and soil bulk density, which are parameters needed to obtain the upper and lower limits of LLWR. The S index was obtained from the water retention curve. The relative density was obtained from the relationship between bulk density and maximum density obtained from the Proctor test. The S index varied as a function of soil management. The variation in LLWR differed between the studied areas as a function of soil bulk density. The relative densities for NV1 and NV2 were lower than for cultivated areas, showing that intensive soil use has caused compaction. The studied parameters seem to be good indicators of soil physical quality, and it was noticed that soils under cultivation suffer an alteration of their structure relative to soils under natural vegetation.
机译:近年来,人们对土壤物理质量的关注日益增加,特别是考虑到由于大量使用土壤而引起的严重问题。我们假设灌溉区域的土壤管理不当会破坏巴西东北部某些地区的敏感土壤结构。这项研究的目的是评估与一年四季作物和多年生作物相比,巴西塞阿拉州自然植被下的灌溉土壤的物理质量。测量了最小极限水范围(LLWR),S指数和相对密度。在四个耕种区(香蕉,番石榴,牧场和玉米/豆类)和两个与耕作相邻的自然植被区(NV1,NV2)的两个深度(5-10和20-25 cm)处采集未受干扰的土壤样品地区。所有地点都在巴西塞阿拉的北利莫埃罗的Jaguaribe-Apodi灌溉区。使用保水曲线,土壤的抗渗透性和土壤容重来确定LLWR,这是获得LLWR上限和下限所需的参数。从保水曲线获得S指数。从堆积密度和从Proctor试验获得的最大密度之间的关系获得相对密度。 S指数随土壤管理而变化。 LLWR的变化在研究区域之间随土壤容重的变化而不同。 NV1和NV2的相对密度低于耕种区,表明密集​​的土壤使用已导致压实。研究的参数似乎是土壤物理质量的良好指标,并且注意到耕作土壤相对于天然植被下的土壤结构发生了变化。

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