Effects of mulching on soil physical properties and runoff under semi-arid conditions in southern Spain

被引:415
作者
Jordan, Antonio [1 ]
Zavala, Lorena M. [1 ]
Gil, Juan [2 ]
机构
[1] Univ Seville, Fac Quim, Dept Cristalog Mineral & Quim Agr, Seville 41012, Spain
[2] Univ Cordoba, Fac Ciencias, Dept Quim Agr & Edafol, Cordoba 14014, Spain
关键词
Aggregate stability; Bulk density; Mulching; No till; Simulated rainfall; Soil loss; Soil structure; Southern Spain; ROCK FRAGMENT COVER; ORGANIC-MATTER; AGGREGATE STABILITY; LONG-TERM; CARBON SEQUESTRATION; CONSERVATION TILLAGE; RESIDUE MANAGEMENT; NITROGEN STORAGE; CROPPING SYSTEMS; BULK-DENSITY;
D O I
10.1016/j.catena.2010.01.007
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Application of crop residues to soil and reduced or no tillage are current management practices in order to achieve better water management, increase soil fertility, crop production and soil erosion control. This study was carried out to quantify the effect of wheat straw mulching in a no tilled Fluvisol under semi-arid conditions in SW Spain and to determine the optimum rate in terms of cost and soil protection. After a 3-years experiment, mulching application significantly improved physical and chemical properties of the studied soil with respect to control, and the intensity of changes was related to mulching rate. The organic matter content was generally increased, although no benefit was found beyond 10 Mg ha(-1) year(-1). Bulk density, porosity and aggregate stability were also improved with increasing mulching rates, which confirmed the interactions of these properties. Low mulching rates did not have a significant effect on water properties with respect to control, although the available water capacity increased greatly under high mulching rates. After simulated rainfall experiments (65 mm h(-1) intensity), it was found that the mulch layer contributed to increase the roughness and the interception of raindrops, delaying runoff generation and enhancing the infiltration of rain water during storms. Mulching contributed to a reduction in runoff generation and soil losses compared to bare soil, and negligible runoff flow or sediment yield were determined under just 5 Mg ha(-1) year(-1) mulching rate. It was observed that during simulations, the erosive response quickly decreases with time after prolonged storms (30 min) due to the exhaustion of available erodible particles. These results suggest that the erosive consequences of intermediate intensity 5-years-recurrent storms in the studied area could be strongly diminished by using just 5 Mg ha(-1) year mulching rates. (C) 2010 Elsevier B.V. All rights reserved.
引用
收藏
页码:77 / 85
页数:9
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