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Divergent controls of exchangeable calcium and iron oxides in regulating soil organic carbon content across climatic gradients in arid regions

文献类型： 外文期刊

作者： Wang, Zhufeng 1 ; Jing, Xin 3 ; Lin, Litao 4 ; Wang, Yugang 5 ; Feng, Wenting 2 ;

作者机构： 1.Chinese Acad Agr Sci, Inst Agr Resources & Reg Planning, State Key Lab Efficient Utilizat Arid & Semiarid A, Beijing 100081, Peoples R China

2.Beijing Forestry Univ, Sch Grassland Sci, Beijing 100083, Peoples R China

3.Lanzhou Univ, Coll Pastoral Agr Sci & Technol, State Key Lab Herbage Improvement & Grassland Agro, Lanzhou 730020, Gansu, Peoples R China

4.Chinese Res Inst Environm Sci, Ctr Ecol Civilizat Res, Beijing 100012, Peoples R China

5.Chinese Acad Sci, Xinjiang Inst Ecol & Geog, State Key Lab Desert & Oasis Ecol, Urumqi 830011, Xinjiang, Peoples R China

6.Chinese Acad Sci, Fukang Stn Desert Ecol, Fukang 831505, Xinjiang, Peoples R China

关键词： Arid regions; Climate; Elevational gradient; Geochemical properties; Mountain systems; Organic-mineral association

期刊名称：AGRICULTURAL AND FOREST METEOROLOGY （ 影响因子：6.2； 五年影响因子：6.9 ）

ISSN： 0168-1923

年卷期： 2024 年 349 卷

页码：

收录情况： SCI

摘要： Elevational gradients offer powerful natural experiments for testing how soil organic carbon (SOC) responds to environmental changes (e.g., climate, plant inputs, and soil geochemistry) across a wide range. Exchangeable calcium (Ca ex ) emerges as an important geochemical driving factor of SOC content in arid regions, yet its significance in regulating SOC content across climatic gradients remains poorly understood. Here, we assessed the relative importance of climate variables, plant inputs, and geochemical properties in controlling SOC content along a 2,500-m elevational gradient in the Tianshan Mountains. We explored the roles of Ca ex in regulating the interactions between iron (Fe)-(hydro)oxides and SOC content. We found that soil Ca ex (i.e., Na 2 SO 4 -extracted), likely controlled by biological cycling, was the major contributor to SOC content in cold and wet climatic conditions (1,400 - 3,035 m a.s.l.), where soils had relatively high Fe o and low pH (5.8-7.9). In contrast, amorphous Fe, not Ca ex , was the most important regulator for SOC content in warm and dry climatic conditions (481 - 1,240 m a.s.l.) with Ca-rich and high pH soils (7.6-9.0). Moreover, the results of partial correlation analysis suggested that Ca ex competed with Fe-(hydro)oxides in modulating SOC content in cold and wet climatic conditions due to low soil pH, but facilitated SOC stabilization by Fe-(hydro)oxides in warm and dry climatic conditions. Although climatic variables and plant inputs were significantly associated with SOC content, our findings indicated that Ca ex and Fe-(hydro)oxides had divergent controls over SOC content across climatic gradients in arid regions, depending on soil pH level. Our study reveals new insights on the potential role of cations in complexation of organic matter with minerals across a wide range of environmental conditions in the field.

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