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Journal ArticleDOI

Soil organic carbon dynamics jointly controlled by climate, carbon inputs, soil properties and soil carbon fractions

TLDR
The direct correlation of rC with climate was significantly weakened if removing the effects of soil properties and C pools, and vice versa, and the complex interconnections in regulating SOC dynamics are revealed.
Abstract
Soil organic carbon (SOC) dynamics are regulated by the complex interplay of climatic, edaphic and biotic conditions However, the interrelation of SOC and these drivers and their potential connection networks are rarely assessed quantitatively Using observations of SOC dynamics with detailed soil properties from 90 field trials at 28 sites under different agroecosystems across the Australian cropping regions, we investigated the direct and indirect effects of climate, soil properties, carbon (C) inputs and soil C pools (a total of 17 variables) on SOC change rate (rC, Mg C ha−1 yr−1) Among these variables, we found that the most influential variables on rC were the average C input amount and annual precipitation, and the total SOC stock at the beginning of the trials Overall, C inputs (including C input amount and pasture frequency in the crop rotation system) accounted for 27% of the relative influence on rC, followed by climate 25% (including precipitation and temperature), soil C pools 24% (including pool size and composition) and soil properties (such as cation exchange capacity, clay content, bulk density) 24% Path analysis identified a network of intercorrelations of climate, soil properties, C inputs and soil C pools in determining rC The direct correlation of rC with climate was significantly weakened if removing the effects of soil properties and C pools, and vice versa These results reveal the relative importance of climate, soil properties, C inputs and C pools and their complex interconnections in regulating SOC dynamics Ignorance of the impact of changes in soil properties, C pool composition and C input (quantity and quality) on SOC dynamics is likely one of the main sources of uncertainty in SOC predictions from the process-based SOC models

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Citations
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Journal ArticleDOI

Responses of soil carbon sequestration to climate-smart agriculture practices: A meta-analysis.

TL;DR: A meta-analysis of 3,049 paired measurements from 417 peer-reviewed articles demonstrated that, through adopting CSA practices, cropland could be an improved carbon sink and highlighted the importance of considering local environmental factors in identifying appropriate CSA Practices for mitigating greenhouse gas emissions while ensuring crop productivity.
Journal ArticleDOI

Climate and plant controls on soil organic matter in coastal wetlands.

TL;DR: The results indicate that future changes in SOM and plant productivity, regulated by cascading effects of precipitation on freshwater availability and salinity, could impact wetland stability and affect the supply of some wetland ecosystem services.
Journal ArticleDOI

Conservation agriculture practices increase soil microbial biomass carbon and nitrogen in agricultural soils: A global meta-analysis

TL;DR: In this paper, the authors evaluated the influence of conservation agriculture practices on soil microbial biomass C (Cmic) and nitrogen (Nmic), and the microbial quotient (qMIC, Cmic-to-organic C ratio), on a global scale using meta-analysis based on data from 96 recent publications.
Journal ArticleDOI

Global subsoil organic carbon turnover times dominantly controlled by soil properties rather than climate.

TL;DR: It is found that temperature and in general climate effects are secondary to effects due to soil properties at both local and global scales—this now needs to be regarded for diagnosing subsoil SOC dynamics.
Journal ArticleDOI

Climate, carbon content, and soil texture control the independent formation and persistence of particulate and mineral-associated organic matter in soil

TL;DR: In this article, the formation and persistence of newly-formed soil organic matter (SOM) is investigated in 10 agricultural sites in Canada, and the authors found that the formation of SOM and the degree to which it is protected from decomposition are important for determining the long-term persistence of SOM.
References
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Journal ArticleDOI

Soil carbon sequestration impacts on global climate change and food security.

TL;DR: In this article, the carbon sink capacity of the world’s agricultural and degraded soils is 50 to 66% of the historic carbon loss of 42 to 78 gigatons of carbon.
Journal ArticleDOI

Temperature sensitivity of soil carbon decomposition and feedbacks to climate change

TL;DR: This work has suggested that several environmental constraints obscure the intrinsic temperature sensitivity of substrate decomposition, causing lower observed ‘apparent’ temperature sensitivity, and these constraints may, themselves, be sensitive to climate.
Journal ArticleDOI

A working guide to boosted regression trees

TL;DR: This study provides a working guide to boosted regression trees (BRT), an ensemble method for fitting statistical models that differs fundamentally from conventional techniques that aim to fit a single parsimonious model.
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Stabilization mechanisms of soil organic matter: Implications for C-saturation of soils

TL;DR: The relationship between soil structure and the ability of soil to stabilize soil organic matter (SOM) is a key element in soil C dynamics that has either been overlooked or treated in a cursory fashion when developing SOM models as discussed by the authors.
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