文献类型： 外文期刊

作者： Yang, Yonghui ¹ ; Wu, Jicheng ¹ ; Zhao, Shiwei ³ ; Mao, Yongping ⁴ ; Zhang, Jiemei ¹ ; Pan, Xiaoying ¹ ; He, Fang ¹ ; van ¹ ;

作者机构： 1.Henan Acad Agr Sci, Inst Plant Nutr & Resource Environm, Zhengzhou 450002, Peoples R China

2.Minist Agr, Yuanyang Expt Stn Crop Water Use, Yuanyang, Peoples R China

3.Northwest A&F Univ, Inst Soil & Water Conservat, Yangling, Shaanxi, Peoples R China

4.Gen Hosp Jinshui Dist Zhengzhou, Zhengzhou, Peoples R China

5.Wageningen Univ & Res, Hydrol & Quantitat Water Management Grp, Wageningen, Netherlands

关键词： soil organic carbon; soil physical properties; soil pores; sub‐ soiling; X‐ ray CT scan

期刊名称：LAND DEGRADATION & DEVELOPMENT （ 影响因子：3.775； 五年影响因子：4.162 ）

ISSN： 1085-3278

年卷期：

页码：

收录情况： SCI

摘要： Long-term conventional tillage leads to soil compaction and formation of a plough layer, which affects soil physical properties, transport of water, and growth of crop roots toward deeper soil, resulting in soil degradation and a decline in crop productivity. Long-term sub-soiling tillage has proven to be an effective measure for remediating the plough layer and improving the structure and physical properties of the soil. In this study, we experimentally investigated the effects of long-term sub-soiling tillage in an arid region of Henan Province, China, along a deep soil (0-100 cm) profile over 8 years of sub-soiling tillage at a depth of 30 cm and compared the results against conventional tillage at a depth of 15 cm. We measured soil pore distributions of macropores (> 1 mm in diameter), mesopores (0.16-1.0 mm), and total pores (> 0.16 mm) measured by X-ray computed tomography (CT), soil total porosity (phi) and > 0.16 mm equivalent porosity measured by conventional methods, soil bulk density (rho(s)), soil organic carbon content (SOC), the proportion of macroaggregates (> 0.25 mm) (PMA), soil field moisture capacity (fc), available moisture content, and saturated hydraulic conductivity (K-sat). The results indicate that long-term sub-soiling tillage increased soil pore numbers at 0-35 cm depth (macropores, mesopores, and total pores), improved pore shape, and significantly increased porosity at 0-20 cm depth (macropores, mesopores, and total pores; p < 0.05) compared to conventional tillage. In addition, phi and > 0.16 mm equivalent porosity were increased by 10.4 and 87.1% at depths of 0-60 cm under sub-soiling tillage, respectively. SOC (0-55 cm depth), fc (0-45 cm depth), available moisture content (0-40 cm depth), K-sat (0-40 cm depth), and PMA (0-50 cm depth) were increased by 16.7, 14.3, 23.8, 471.5, and 98.3%, respectively, and rho(s) (0-60 cm depth) was reduced by 8.6%. Observed correlations between SOC, soil pore parameters, and soil physical properties suggest that soil pore parameters and soil physical properties can be improved by increasing SOC. These correlations are stronger under sub-soiling than that under conventional tillage. Therefore, sub-soiling is an effective technique for improving soil pore characteristics and physical properties while preventing soil degradation.