耕作方法、残留物水平和前进速度对土壤水分特征曲线(SWCC)的短期影响:以伊朗胡齐斯坦省卡伦河东部土壤为例。

Desert Pub Date : 2019-12-01 DOI:10.22059/JDESERT.2019.76387
A. Shojaee, B. Khalilimoghaddam, F. Moradi
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引用次数: 1

摘要

本研究旨在调查一个作物年(2014-2015年)内耕作方法、残留率和前进速度对Haploustepts土壤水分特征曲线(SWCC)的影响。处理包括常规机械化耕作(CT:犁板犁+圆盘)和减少耕作(RT1:凿-peker+犁和RT2:组合耕作),不同的地表残留物,包括无残留物、40%残留物和80%残留物三个级别,以及三个级别的前进速度:低(4km/h)、正常(7km/h)和高(10km/h)。将实验保水数据拟合到单模态van Genuchten(称为单模态vG)和双模态Dexter(称为双模态Dex)模型中。除参数n外,未观察到对不同物理参数的显著影响。在SWCC拐点的斜率中,与RT2相比,CT和RT1治疗分别减少了11.8%和8.9%。根据结果,CT下测得的结果往往高于其他耕作处理。剩余的掩护和更高的前进速度往往会增加和。PSD的变化在较大(宏观)和中等(细观)孔径类别中更为明显。在RT2中观察到作为透射孔的结构空隙率的最高值。这一发现表明,关于、和值,土壤PSD描述系统是一个双峰分布,如H-L;因此,由于土壤结构的层次性,van-Genuchten方程不能很好地描述多模态土壤。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Short-term effect of tillage methods, residue levels, and forward speeds on soil-water characteristic curve (SWCC): A case study on the eastern soils of Karun River, Khuzestan province, Iran.
The current study was conducted to investigate the effect of tillage methods, residue rates, and forward speeds on the soil-water characteristic curve (SWCC) of Haploustepts soil over the course of one crop year (2014-2015). The treatments consisted of conventional mechanized tillage (CT: moldboard plough+disc) and reduced tillage (RT1: chisel peker+plough and RT2: combined tillage), different surface residues, including three levels of no residue, 40% residue, and 80% residue, and forward speeds at three levels: low (4 km/h), normal (7 km/h), and high (10 km/h). The experimental water retention data were fitted to uni-modal van Genuchten (termed uni-modal vG) and bi-modal Dexter (termed bi-modal Dex) models. No significant impact was observed on different physical parameters, except for parameter n. In the slope at the inflection point of SWCC, 11.8% and 8.9% reductions were observed in CT and RT1 treatments, respectively, compared to RT2. Based on the results,  measured under CT tended to be higher than that of other tillage treatments. Residual covers and higher forward speeds tended to increase both  and . Changes in PSD were more pronounced in larger (macro) and medium (meso) pore diameter classes. The highest value of structural void ratio as transmission pores was observed in RT2. This finding indicates that with respect to , , , and  values, the soil PSD descriptive system is a bi-peak distribution such as H-L; therefore, due to the hierarchical nature of soil structure, van Genuchten equation cannot appropriately describe multi-modal soils inherently.
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