Geographic Distribution Pattern Determines Soil Microbial Community Assembly Process in Acanthopanax senticosus Rhizosphere Soil DOI Creative Commons
Mingyu Wang, Xiangyu Xing,

Youjia Zhang

et al.

Microorganisms, Journal Year: 2024, Volume and Issue: 12(12), P. 2506 - 2506

Published: Dec. 4, 2024

The geographic distribution patterns of soil microbial communities associated with cultivated Acanthopanax senticosus plants in Northeast China were investigated. High-throughput sequencing revealed that the diversity and community assembly bacterial fungal inter-root varied significantly location. study found predominantly assembled through stochastic processes at most sites, while showed greater variation, both deterministic involved. complexity bacterial-fungal co-occurrence networks also longitude latitude, demonstrating positive negative interactions. PICRUSt 2.0 FUNGuild used to predict potential functions microbiota, respectively, during different land use patterns. average taxonomic distinctness (AVD) index indicated varying degrees stability across sites. Key taxa contributing variability identified Random Forest modeling, Bacteriap25 Sutterellaceae standing out among bacteria, Archaeorhizomyces Clavaria fungi. Soil chemical properties, including pH, TN, TP, EC, SOC, correlated diversity, composition, networks. Structural equation modeling directly indirectly influenced properties communities. Overall, provides insights into A. highlights need for further research underlying mechanisms shaping these

Language: Английский

Reduced accrual of mineral-associated organic matter after two years of enhanced rock weathering in cropland soils, though no net losses of soil organic carbon DOI Creative Commons
Noah W. Sokol, Jaeeun Sohng, Kimber Moreland

et al.

Biogeochemistry, Journal Year: 2024, Volume and Issue: 167(8), P. 989 - 1005

Published: July 23, 2024

Abstract Enhanced rock weathering (ERW), the application of crushed silicate to soil, can remove atmospheric carbon dioxide by converting it (bi) carbonate ions or solid minerals. However, few studies have empirically evaluated ERW in field settings. A critical question remains as whether additions might positively negatively affect soil organic matter (SOM)—Earth’s largest terrestrial (C) pool and a massive reservoir nitrogen (N). Here, three irrigated cropland trials California, USA, we investigated effect meta-basalt on different pools (i.e., mineral-associated matter, MAOM, particulate POM), active microbial biomass, community composition. After 2 years additions, MAOM stocks were lower upper surface (0–10 cm) plots with compared unamended control plots. At sites where baseline pre-treatment data available, neither total SOC nor SON decreased over study accrual rate MAOM-C MAOM-N at 0–10 cm was vs. controls. Before is deployed large scales, our results suggest that should assess effects SOM pools, especially multi-year time scales environmental contexts, accurately changes net C understand mechanisms driving interactions between cycling.

Language: Английский

Citations

5

Parameters of labile organic carbon as the indicators of the stability of soil organic matter under different land use DOI Creative Commons
Erika Balontayová, Juraj Hreško, Viera Petlušová

et al.

Soil and Water Research, Journal Year: 2025, Volume and Issue: unknown

Published: Jan. 3, 2025

The labile fractions of organic carbon (OC), which are a reflection the properties soil and its use, appear to be suitable parameters for their use as indicators. aim this study was determine reliable relatively simple indicators detecting chemical physical stabilizations OC, would respond sensitively land use. includes forest ecosystem (FE) agroecosystem (AE) with different tillage intensities (reduced tillage, RT conventional CT) on real farms. Parameters C N were tested. For depth < 0.1 m in FE, hot water extractable (HWEOC) stabilization nitrogen (NL) most Higher values HWEOC indicate OC by decreasing decomposition, pH or increasing carbonates, recalcitrant fractions, higher NL incorporation into silt fraction larger macro-aggregates. In AE RT, these pool index (CPI) lability (LIC) stabilization. CPI LIC formation size-optimal dry-sieved (DSA; 1–3 mm) wet-sieved (WSA; 1–2 aggregates. CT, it NL. Its point through alkaline cations, size-fraction > 0.01 mm DSA (1–3 mm). 0.3 AE, CL (for RT), value points clay CT), indicates conditions acidification.

Language: Английский

Citations

0

Impact of long-term drip irrigation on soil organic carbon and nutrient stocks in arid oasis farmlands DOI

Weihao Sun,

Zhibin He,

Bing Liu

et al.

CATENA, Journal Year: 2025, Volume and Issue: 252, P. 108895 - 108895

Published: March 5, 2025

Language: Английский

Citations

0

Terracing stabilizes and enhances soil organic carbon sequestration benefits of revegetation on the Loess Plateau, China DOI

Hui Cheng,

Hao Feng,

Xiaoping Zhang

et al.

CATENA, Journal Year: 2025, Volume and Issue: 255, P. 109018 - 109018

Published: April 9, 2025

Language: Английский

Citations

0

Reduced accrual of mineral-associated organic matter after two years of enhanced rock weathering in cropland soils, though no net losses of soil organic carbon DOI
Noah W. Sokol, Jaeeun Sohng, Kimber Moreland

et al.

bioRxiv (Cold Spring Harbor Laboratory), Journal Year: 2024, Volume and Issue: unknown

Published: June 27, 2024

Abstract Enhanced rock weathering (ERW), the application of crushed silicate to soil, can remove atmospheric carbon dioxide by converting it (bi)carbonate ions or solid carbonate minerals. However, few field studies have empirically evaluated ERW in settings. A critical question remains as whether additions might positively negatively affect soil organic matter (SOM) – Earth’s largest terrestrial (C) pool and a massive reservoir nitrogen (N). Here, three irrigated cropland sites California, USA, we investigated effect meta-basalt on different pools (i.e., mineral-associated particulate matter), active microbial biomass, community composition. After two years additions, (MAOM) stocks were lower upper surface (0-10 cm) compared unamended controls. At where baseline pre-treatment data available, neither total SOC nor SON decreased over study control plots. accrual rate MAOM-C MAOM-N at 0-10 cm was plots with vs. Before is deployed large scales, our results suggest that trials should assess effects SOM pools, especially multi-year time accurately changes net C understand mechanisms driving interactions between cycling.

Language: Английский

Citations

1

Biochar affects soil properties over 1 m depth in an alkaline soil of north China Plain DOI
Xiongxiong Bai,

Jiao Tang,

Qingwei Lin

et al.

Journal of Environmental Management, Journal Year: 2024, Volume and Issue: 370, P. 123097 - 123097

Published: Oct. 30, 2024

Language: Английский

Citations

1

Ecosystem Carbon Stock in Iron-Metamorphic Soils with Different Types of Land Use in South Karelia DOI
И. А. Дубровина, Е. В. Мошкина, A. V. Tuyunen

et al.

Eurasian Soil Science, Journal Year: 2024, Volume and Issue: 57(10), P. 1567 - 1578

Published: Oct. 1, 2024

Language: Английский

Citations

0

Geographic Distribution Pattern Determines Soil Microbial Community Assembly Process in Acanthopanax senticosus Rhizosphere Soil DOI Creative Commons
Mingyu Wang, Xiangyu Xing,

Youjia Zhang

et al.

Microorganisms, Journal Year: 2024, Volume and Issue: 12(12), P. 2506 - 2506

Published: Dec. 4, 2024

The geographic distribution patterns of soil microbial communities associated with cultivated Acanthopanax senticosus plants in Northeast China were investigated. High-throughput sequencing revealed that the diversity and community assembly bacterial fungal inter-root varied significantly location. study found predominantly assembled through stochastic processes at most sites, while showed greater variation, both deterministic involved. complexity bacterial-fungal co-occurrence networks also longitude latitude, demonstrating positive negative interactions. PICRUSt 2.0 FUNGuild used to predict potential functions microbiota, respectively, during different land use patterns. average taxonomic distinctness (AVD) index indicated varying degrees stability across sites. Key taxa contributing variability identified Random Forest modeling, Bacteriap25 Sutterellaceae standing out among bacteria, Archaeorhizomyces Clavaria fungi. Soil chemical properties, including pH, TN, TP, EC, SOC, correlated diversity, composition, networks. Structural equation modeling directly indirectly influenced properties communities. Overall, provides insights into A. highlights need for further research underlying mechanisms shaping these

Language: Английский

Citations

0