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Physical quality of a Luvisol under agroforestry systems in a semi-arid region, Brazil

机译:巴西半干旱地区农林业系统下Luvisol的物理质量

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Agroforestry systems provide many environmental benefits in semi-arid regions; however, trampling by cattle, and agricultural practices, can degrade physical quality of the soil. The aim of this study was to evaluate the degree of compaction and the compression behaviour of a Luvisol after 14 years under agro-silvopastoral (ASP) and silvopastoral systems (SILV), compared with a soil under natural vegetation (NV). We evaluated the degree of soil compactness, compaction index, pre-consolidation pressure, maximum bulk density, critical water content and the stocks of total organic carbon (C), organic matter (OM), C in light organic matter (LOM), and nitrogen (N) in LOM. The results indicated that agroforestry systems change the compressive behaviour of the soil, increasing maximum bulk density (P < 0.05) and reducing critical water content (P < 0.05). Despite the increases in maximum bulk density, changes induced by agroforestry system did not affect the pore space, as shown by similar values for degree of compactness (P > 0.05) under ASP, SILV and NV. This suggests a change in the quality of OM, as evidenced by the lower values for stocks of N in LOM (P < 0.10) and total organic C (P < 0.05) under ASP and SILV, whereas pre-consolidation pressure was unaffected (P > 0.05). After 14 years, the degree of compactness and load-bearing capacity of the soils under ASP and SILV had not increased, being suitable for plant growth.
机译:农林系统为半干旱地区带来了许多环境效益;但是,用牛践踏和农业实践会降低土壤的物理质量。这项研究的目的是评估与天然植被(NV)下的土壤相比,Luvisol在农用农牧农(ASP)和农牧农牧系统(SILV)下14年后的压实度和压缩行为。我们评估了土壤压实度,压实指数,预固结压力,最大堆积密度,临界水含量以及总有机碳(C),有机物(OM),轻有机物中的C(LOM)和LOM中的氮(N)。结果表明,农林业系统改变了土壤的压缩行为,增加了最大容重(P <0.05)并降低了临界水分含量(P <0.05)。尽管最大堆密度增加,但农林系统引起的变化并未影响孔隙空间,如ASP,SILV和NV下的紧密度相似值(P> 0.05)所示。这表明OM的质量发生了变化,这可以通过ASP和SILV下LOM中的N储量(P <0.10)和总有机碳(P <0.05)较低的值来证明,而预固结压力不受影响(P > 0.05)。 14年后,ASP和SILV下土壤的致密性和承重能力没有增加,适合植物生长。

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