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Least limiting water range and S index to evaluate some soil physical quality in the northeast Brazil

机译:最小限制水分和S指数,以评估巴西东北部的一些土壤体质

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The concern with soil physical quality has grown in recent years, particularly due to serious problems caused by soil use. The objective of this research was to evaluate the soil physical quality of irrigated areas in the State of Ceara, Brazil, through the use of the Least limiting Water Range (LLWR) and the S index. Undisturbed soil samples were collected at 5-10cm depth in three areas, natural vegetation (NV), area under banana cultivation (B) and a pasture area (P), all located in Jaguaribe-ApodiIrrigated District, Limoeiro do Norte, Ceara, Brazil. The LLWR was determined using the water retention curve, the soil resistance to penetration and soil bulk density, parameters needed to obtain the upper and lower limit. The S index was obtained fromthe water retention curve. The S index was sensitive to soil structure alterations caused probably by tillage. The variation of the LLWR differed between the studied areas as a function of the soil bulk density. The LLWR and S index seem to be good indicators of soil physical quality, and it was noticed that soils under cultivation suffer an alteration of their structure compared to soils under natural vegetation.
机译:近年来,土壤体质质量的担忧尤其是由于土壤利用引起的严重问题。本研究的目的是通过使用最小限制的水范围(LLWR)和S指数,评估CEARA状态下的灌溉区域的土壤身体质量。在三个区域,天然植被(NV),香蕉种植​​面积(b)和牧场地区(p)下,所有位于Jaguaribe-Apodiored地区,Limoeiro Do Norte,Cara,巴西北部北部地区(P),牧草地区(B)下,收集了未受干扰的土壤样品。使用水保持曲线测定LLWR,对渗透和土壤堆积密度的土壤抗性,获得上限和下限所需的参数。 S指数从水保持曲线获得。 S指数对可能由耕作引起的土壤结构改变敏感。作为土壤堆积密度的函数,LLWR的变化不同。 LLWR和S指数似乎是土壤体质的良好指标,并注意到培养的土壤与天然植被下的土壤相比,它们的结构遭受了结构的改变。

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