Rubber plant root properties induce contrasting soil aggregate stability through cohesive force and reduced land degradation risk in southern China

IF 5.8 2区 农林科学 Q1 SOIL SCIENCE
Soil Pub Date : 2024-12-16 DOI:10.5194/egusphere-2024-3602
Waqar Ali, Amani Milinga, Tao Luo, Mohammad Nauman Khan, Asad Shah, Khurram Shehzad, Qiu Yang, Huai Yang, Wenxing Long, Wenjie Liu
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Abstract

Abstract. In southern China, Hainan Island faces land degradation risks due to poor soil physical properties, such as a high proportion of microaggregates (< 0.25 mm), low soil organic matter (SOM) content, and frequent uneven rainfall. The cohesive force between soil particles, which is influenced by plant root properties and root-derived SOM, is essential for improving soil aggregate stability and mitigating land degradation. However, the mechanisms by which rubber root properties and root-derived SOM affect soil aggregate stability through cohesive forces in tropical regions remain unclear. This study compared rubber plants of varying ages to assess the effects of root properties and root-derived SOM on soil aggregate stability and cohesive forces. Older rubber plants (> 11-years-old) showed greater root diameters (RD) (0.81–0.91 mm), higher root length (RL) densities (1.83–2.70 cm/cm3), and increased proportions of fine (0.2–0.5 mm) and medium (0.5–1 mm) roots, leading to higher SOM due to lower lignin and higher cellulose contents. Older plants exhibited higher soil cohesion, with significant correlations among root characteristics, SOM, and cohesive force, whereas the random forest (RF) model identified aggregates (> 0.25 mm), root properties, SOM, and cohesive force as the key factors influencing mean weight diameter (MWD) and geometric mean diameter (GMD). Furthermore, partial least squares-path models (PLS-PM) showed that the RL density (RLD) directly influenced SOM (path coefficient 0.70) and root-free cohesive force (RFCF) (path coefficient 0.30), which in turn affected the MWD, with additional direct RLD effects on the SOM (path coefficient 0.45) and MWD (path coefficient 0.64) in the surface soil. Cohesive force in rubber plants of different ages increased macroaggregates (> 0.25 mm) and decreased microaggregates (< 0.25 mm), with topsoil average MWD following the order: CK (0.98 mm) < 5Y_RF (1.26 mm) < MF (1.31 mm) < 11Y_RF (1.36 mm) < 27Y_RF (1.48 mm) < 20Y_RF (1.51 mm). Rubber plant root properties enhance soil aggregate stability and reduce the land degradation risk in tropical regions.
橡胶植物根系的特性通过内聚力诱导对比强烈的土壤集聚稳定性,降低中国南方的土地退化风险
摘要在中国南部,海南岛由于土壤物理性质较差,如微集料(< 0.25 mm)比例高、土壤有机质(SOM)含量低以及降雨量不均等原因,面临着土地退化的风险。土壤颗粒之间的内聚力受植物根系特性和根系衍生的 SOM 影响,对于改善土壤团聚稳定性和缓解土地退化至关重要。然而,橡胶根系特性和根系衍生的 SOM 通过内聚力影响热带地区土壤团聚稳定性的机制仍不清楚。本研究比较了不同树龄的橡胶植株,以评估根系特性和根系衍生的 SOM 对土壤聚合稳定性和内聚力的影响。树龄较大的橡胶植株(> 11年)表现出更大的根径(RD)(0.81-0.91毫米)、更高的根长(RL)密度(1.83-2.70厘米/立方厘米)以及更高的细根(0.2-0.5毫米)和中根(0.5-1毫米)比例,由于木质素含量较低和纤维素含量较高,因此SOM较高。老龄植株表现出更高的土壤内聚力,根系特征、SOM 和内聚力之间存在显著相关性,而随机森林(RF)模型则确定聚合体(> 0.25 毫米)、根系特性、SOM 和内聚力是影响平均重量直径(MWD)和几何平均直径(GMD)的关键因素。此外,偏最小二乘法路径模型(PLS-PM)显示,RL 密度(RLD)直接影响 SOM(路径系数 0.70)和无根内聚力(RFCF)(路径系数 0.30),进而影响 MWD,RLD 还直接影响表层土壤中的 SOM(路径系数 0.45)和 MWD(路径系数 0.64)。不同树龄橡胶植株的粘结力增加了大集料(0.25 毫米),减少了微集料(0.25 毫米),表层土壤的平均 MWD 依次为:CK(0.98 毫米);CK(0.98 毫米);CK(0.98 毫米);CK(0.25 毫米);CK(0.25 毫米);CK(0.25 毫米):CK(0.98 毫米);5Y_RF(1.26 毫米);MF(1.31 毫米);11Y_RF(1.36 毫米);27Y_RF(1.48 毫米);20Y_RF(1.51 毫米)。橡胶植物根系的特性增强了热带地区土壤的聚合稳定性,降低了土地退化的风险。
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来源期刊
Soil
Soil Agricultural and Biological Sciences-Soil Science
CiteScore
10.80
自引率
2.90%
发文量
44
审稿时长
30 weeks
期刊介绍: SOIL is an international scientific journal dedicated to the publication and discussion of high-quality research in the field of soil system sciences. SOIL is at the interface between the atmosphere, lithosphere, hydrosphere, and biosphere. SOIL publishes scientific research that contributes to understanding the soil system and its interaction with humans and the entire Earth system. The scope of the journal includes all topics that fall within the study of soil science as a discipline, with an emphasis on studies that integrate soil science with other sciences (hydrology, agronomy, socio-economics, health sciences, atmospheric sciences, etc.).
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