首页> 外文期刊>Land Degradation and Development >CONSERVATION AGRICULTURE HAD A POOR IMPACT ON THE SOIL POROSITY OF VENETO LOW-LYING PLAIN SILTY SOILS AFTER A 5-YEAR TRANSITION PERIOD
【24h】

CONSERVATION AGRICULTURE HAD A POOR IMPACT ON THE SOIL POROSITY OF VENETO LOW-LYING PLAIN SILTY SOILS AFTER A 5-YEAR TRANSITION PERIOD

机译:5年后的过渡期后,保护农业对威尼托低洼普通粉质土壤的土壤孔隙率的影响很差

获取原文
获取原文并翻译 | 示例
           

摘要

Conservation agriculture practices have been proposed as a set of techniques for improving soil structure properties and related ecosystem services. This study compared conservation agriculture (CA) practices (no-tillage, cover crop and residue retention) and conventional intensive tillage system in order to evaluate their effects on total porosity, pore size distribution, pore architecture and morphology. The experiment was set up in 2010 on four farms of the low-lying Veneto Region plain characterized by silty soils. Almost hundred soil samples were collected in 2015 at four depths down to 50-cm layer and investigated for porosity from micrometre (0.0074 mu m) to macrometre (2.5 mm) by coupling mercury intrusion porosimetry and X-ray computed microtomography (mu CT). Indices of soil morphology and architecture were derived by analysing 3D images and mercury intrusion porosimetry pore size curves. Results suggested that silty soils of Veneto plain are microstructured because much (82%) of the porosity ranged between 0.0074 and 30 ae m. CA practices positively influenced the ultramicroporosity class (0.1-5 mu m) (1.86E-01 vs 1.67E-01 mu m(3) mu m(-3)) that is strictly linked to soil organic carbon stabilization while no effects were observed in X-ray mu CT porosity domain (> 26 mu m). Silty soils of Veneto plain showed a slow reaction to CA because of the poor aggregate stability and low soil organic carbon. However, the positive response of the ultramicropore fraction indicates that a virtuous cycle was initiated between soil organic carbon and porosity, hopefully leading to well-developed macropore systems and, in turn, enhanced soil functions and ecosystem services. Copyright (C) 2017 John Wiley & Sons, Ltd.
机译:保护农业实践已提出作为改善土壤结构性质和相关生态系统服务的一套技术。该研究比较了保护农业(CA)实践(无耕作,覆盖作物和残留物保留)和常规的强化耕作系统,以评估它们对总孔隙率,孔径分布,孔结构和形态的影响。该实验于2010年在2010年,在粉状土壤的低洼威尼托地区的四个农场上设立。在2015年以四个深度的近似至50厘米的层收集近百种土样品,并通过偶联汞侵入孔孢子瘤和X射线计算的微观图(MU CT)来研究从微米(0.0074μm)到宏观(2.5mm)的孔隙率。通过分析3D图像和汞侵入孔隙率孔径曲线来源的土壤形态和建筑指数。结果表明,威尼托平原的粉质土壤是显微结构的,因为大量(82%)的孔隙率在0.0074至30 AE m之间。 CA实践对超小级数(0.1-5μm)(1.86E-01 vs 1.67E-01 mu m(3)mu m(3)mu m(3))相对于土壤有机碳稳定,而没有观察到任何效果在X射线MU CT孔隙域(>26μm)。由于聚集稳定性和低土壤有机碳,威尼托平原的贫瘠土壤表现出对CA的缓慢反应。然而,超微孔馏分的阳性反应表明,在土壤有机碳和孔隙率之间引发了良性循环,希望导致发育良好的大孔系统,以及增强土壤功能和生态系统服务。版权所有(c)2017年John Wiley& SONS,LTD.

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号