Details
Original language | English |
---|---|
Article number | 108039 |
Journal | CATENA |
Volume | 241 |
Early online date | 15 Apr 2024 |
Publication status | Published - Jun 2024 |
Abstract
Organic amendments are effective in promoting salt leaching, improving availability of nutrients and increasing crop yield in saline soils. However, the effects of the combined application of organic amendments on soil inorganic carbon (SIC) content and its driving mechanisms are unknown. We examined how changes in soil biochemical properties including moisture content, pH value, dissolved ions, soil organic C (SOC), dissolved organic C (DOC), microbial biomass C (MBC), and activities of C- and N-related enzyme due to applying (i) only mineral fertilizers (control; Ctrl) or mineral fertilization in combination with (ii) manure (M); (iii) biofertilizer plus manure (B+M); and (iv) humic acid plus manure (HA+M) modify SIC pool over three years. Organic amendments increased the content of Ca 2+ and HCO 3 – ions, but significantly decreased Na +, Cl −, and SO 4 2− at 0–60 cm soil layers compared to Ctrl. Furthermore, the activities of β-glucosidase (BG), Xylanase (BX), Cellobiosidase (CE), and β-1,4-N-Acetyl-glucosaminidase (NAG) increased at 0–40 cm soil. Partial least squares path model manifested that organic amendment directly accumulated SIC content by increasing Ca 2+ content and the activities of BX and NAG. Additionally, the decrease of Cl − contents under organic amendments favored the increase of MBC and SOC content, which further increased SIC content. Generally, the effects of HA+M were greater than other fertilization managements, which increased the stocks of SIC and total C at 0–60 cm soils by 27 Mg ha −1 and 47 Mg ha −1, respectively. Furthermore, the effect of organic amendments on SIC content is more pronounced below the first 20 cm. Thus, the application of organic amendments is recommended as an appropriate measure to not only improve soil condition for plant growth and SOC accumulation but also to store C as SIC at deeper depths.
Keywords
- Carbon sequestration, Humic acid plus manure, Organic amendment, Saline soils, Soil inorganic carbon
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Earth-Surface Processes
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In: CATENA, Vol. 241, 108039, 06.2024.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - Inorganic carbon accumulation in saline soils via modification effects of organic amendments on dissolved ions and enzymes activities
AU - Song, Jiashen
AU - Zhang, Hongyuan
AU - Zamanian, Kazem
AU - Chang, Fangdi
AU - Yu, Ru
AU - Wang, Jing
AU - Zhou, Jie
AU - Li, Yuyi
N1 - This study was supported by the National Key R&D Program of China (2023YFD2001400), the National Natural Science Foundation of China (No. U23A2054), the Agricultural Science and Technology Innovation Program (ASTIP No. CAAS-ZDRW202407), the earmarked fund for CARS-02-24, “Open the list” in charge of the science and technology project of Ordos (JBGS-2021-001), German Research Foundation (DFG, ZA 1068/4) and Ministry of Science and Culture of Lower-Saxony, Germany (15-76251-2—Stay-8/22- 5947/2022).
PY - 2024/6
Y1 - 2024/6
N2 - Organic amendments are effective in promoting salt leaching, improving availability of nutrients and increasing crop yield in saline soils. However, the effects of the combined application of organic amendments on soil inorganic carbon (SIC) content and its driving mechanisms are unknown. We examined how changes in soil biochemical properties including moisture content, pH value, dissolved ions, soil organic C (SOC), dissolved organic C (DOC), microbial biomass C (MBC), and activities of C- and N-related enzyme due to applying (i) only mineral fertilizers (control; Ctrl) or mineral fertilization in combination with (ii) manure (M); (iii) biofertilizer plus manure (B+M); and (iv) humic acid plus manure (HA+M) modify SIC pool over three years. Organic amendments increased the content of Ca 2+ and HCO 3 – ions, but significantly decreased Na +, Cl −, and SO 4 2− at 0–60 cm soil layers compared to Ctrl. Furthermore, the activities of β-glucosidase (BG), Xylanase (BX), Cellobiosidase (CE), and β-1,4-N-Acetyl-glucosaminidase (NAG) increased at 0–40 cm soil. Partial least squares path model manifested that organic amendment directly accumulated SIC content by increasing Ca 2+ content and the activities of BX and NAG. Additionally, the decrease of Cl − contents under organic amendments favored the increase of MBC and SOC content, which further increased SIC content. Generally, the effects of HA+M were greater than other fertilization managements, which increased the stocks of SIC and total C at 0–60 cm soils by 27 Mg ha −1 and 47 Mg ha −1, respectively. Furthermore, the effect of organic amendments on SIC content is more pronounced below the first 20 cm. Thus, the application of organic amendments is recommended as an appropriate measure to not only improve soil condition for plant growth and SOC accumulation but also to store C as SIC at deeper depths.
AB - Organic amendments are effective in promoting salt leaching, improving availability of nutrients and increasing crop yield in saline soils. However, the effects of the combined application of organic amendments on soil inorganic carbon (SIC) content and its driving mechanisms are unknown. We examined how changes in soil biochemical properties including moisture content, pH value, dissolved ions, soil organic C (SOC), dissolved organic C (DOC), microbial biomass C (MBC), and activities of C- and N-related enzyme due to applying (i) only mineral fertilizers (control; Ctrl) or mineral fertilization in combination with (ii) manure (M); (iii) biofertilizer plus manure (B+M); and (iv) humic acid plus manure (HA+M) modify SIC pool over three years. Organic amendments increased the content of Ca 2+ and HCO 3 – ions, but significantly decreased Na +, Cl −, and SO 4 2− at 0–60 cm soil layers compared to Ctrl. Furthermore, the activities of β-glucosidase (BG), Xylanase (BX), Cellobiosidase (CE), and β-1,4-N-Acetyl-glucosaminidase (NAG) increased at 0–40 cm soil. Partial least squares path model manifested that organic amendment directly accumulated SIC content by increasing Ca 2+ content and the activities of BX and NAG. Additionally, the decrease of Cl − contents under organic amendments favored the increase of MBC and SOC content, which further increased SIC content. Generally, the effects of HA+M were greater than other fertilization managements, which increased the stocks of SIC and total C at 0–60 cm soils by 27 Mg ha −1 and 47 Mg ha −1, respectively. Furthermore, the effect of organic amendments on SIC content is more pronounced below the first 20 cm. Thus, the application of organic amendments is recommended as an appropriate measure to not only improve soil condition for plant growth and SOC accumulation but also to store C as SIC at deeper depths.
KW - Carbon sequestration
KW - Humic acid plus manure
KW - Organic amendment
KW - Saline soils
KW - Soil inorganic carbon
UR - http://www.scopus.com/inward/record.url?scp=85190329131&partnerID=8YFLogxK
U2 - 10.1016/j.catena.2024.108039
DO - 10.1016/j.catena.2024.108039
M3 - Article
VL - 241
JO - CATENA
JF - CATENA
SN - 0341-8162
M1 - 108039
ER -