scholarly journals Rising Temperature May Trigger Deep Soil Carbon Loss Across Forest Ecosystems

2020 ◽  
Vol 7 (19) ◽  
pp. 2001242 ◽  
Author(s):  
Jinquan Li ◽  
Junmin Pei ◽  
Elise Pendall ◽  
Peter B. Reich ◽  
Nam Jin Noh ◽  
...  
Keyword(s):  
Soil Carbon ◽  
Forest Ecosystems ◽  
Carbon Loss ◽  
Deep Soil

scholarly journals Lower soil moisture and deep soil temperatures in thermokarst features increase old soil carbon loss after 10 years of experimental permafrost warming

2020 ◽  
Author(s):  
Elaine F. Pegoraro ◽  
Marguerite E. Mauritz ◽  
Kiona Ogle ◽  
Christopher H. Ebert ◽  
Edward A. G. Schuur
Keyword(s):  
Soil Moisture ◽  
Soil Carbon ◽  
Carbon Loss ◽  
Deep Soil ◽  
Permafrost Warming ◽  
Soil Temperatures

scholarly journals Assessing Wood and Soil Carbon Losses from a Forest-Peat Fire in the Boreo-Nemoral Zone

Forests ◽  
2021 ◽  
Vol 12 (7) ◽  
pp. 880
Author(s):  
Andrey Sirin ◽  
Alexander Maslov ◽  
Dmitry Makarov ◽  
Yakov Gulbe ◽  
Hans Joosten
Keyword(s):  
Soil Carbon ◽  
Stand Structure ◽  
Peat Soil ◽  
Burned Area ◽  
Tree Biomass ◽  
Carbon Loss ◽  
Forest Stand Structure ◽  
Peat Fire ◽  
Peat Fires ◽  
Carbon Losses

Forest-peat fires are notable for their difficulty in estimating carbon losses. Combined carbon losses from tree biomass and peat soil were estimated at an 8 ha forest-peat fire in the Moscow region after catastrophic fires in 2010. The loss of tree biomass carbon was assessed by reconstructing forest stand structure using the classification of pre-fire high-resolution satellite imagery and after-fire ground survey of the same forest classes in adjacent areas. Soil carbon loss was assessed by using the root collars of stumps to reconstruct the pre-fire soil surface and interpolating the peat characteristics of adjacent non-burned areas. The mean (median) depth of peat losses across the burned area was 15 ± 8 (14) cm, varying from 13 ± 5 (11) to 20 ± 9 (19). Loss of soil carbon was 9.22 ± 3.75–11.0 ± 4.96 (mean) and 8.0–11.0 kg m−2 (median); values exceeding 100 tC ha−1 have also been found in other studies. The estimated soil carbon loss for the entire burned area, 98 (mean) and 92 (median) tC ha−1, significantly exceeds the carbon loss from live (tree) biomass, which averaged 58.8 tC ha−1. The loss of carbon in the forest-peat fire thus equals the release of nearly 400 (soil) and, including the biomass, almost 650 tCO2 ha−1 into the atmosphere, which illustrates the underestimated impact of boreal forest-peat fires on atmospheric gas concentrations and climate.

scholarly journals Undervine groundcover substantially increases shallow but not deep soil carbon in a temperate vineyard

2021 ◽  
Vol 313 ◽  
pp. 107362
Author(s):  
Suzanne M. Fleishman ◽  
Hayden W. Bock ◽  
David M. Eissenstat ◽  
Michela Centinari
Keyword(s):  
Soil Carbon ◽  
Deep Soil

scholarly journals Estimating Annual Soil Carbon Loss in Agricultural Peatland Soils Using a Nitrogen Budget Approach

PLoS ONE ◽  
2015 ◽  
Vol 10 (3) ◽  
pp. e0121432 ◽  
Author(s):  
Emilie R. Kirk ◽  
Chris van Kessel ◽  
William R. Horwath ◽  
Bruce A. Linquist
Keyword(s):  
Soil Carbon ◽  
Nitrogen Budget ◽  
Carbon Loss

scholarly journals Comparing soil carbon loss through respiration and leaching under extreme precipitation events in arid and semi-arid grasslands

2017 ◽  
Author(s):  
Ting Liu ◽  
Liang Wang ◽  
Xiaojuan Feng ◽  
Jinbo Zhang ◽  
Tian Ma ◽  
...  
Keyword(s):  
Climate Change ◽  
Soil Carbon ◽  
Extreme Precipitation ◽  
Dissolved Inorganic Carbon ◽  
Precipitation Event ◽  
Carbon Loss ◽  
Research Attention ◽  
Extreme Precipitation Events ◽  
Leaching Loss ◽  
Arid And Semiarid

Abstract. Respiration and leaching are two main processes responsible for soil carbon loss. While the former has received considerable research attention, studies examining leaching processes are limited especially in semiarid grasslands due to low precipitation. Climate change may increase the extreme precipitation event (EPE) frequency in arid and semiarid regions, potentially enhancing soil carbon loss through leaching and respiration. Here we incubated soil columns of three typical grassland soils from Inner Mongolia and Qinghai-Tibetan Plateau and examined the effect of simulated EPEs on soil carbon loss through respiration and leaching. EPEs induced transient increase of soil respiration, equivalent to 32 % and 72 % of the net ecosystem productivity (NEP) in the temperate grasslands (Xilinhot and Keqi) and 7 % in the alpine grasslands (Gangcha). By comparison, leaching loss of soil carbon accounted for 290 %, 120 % and 15 % of NEP at the corresponding sites, respectively, with dissolved inorganic carbon (DIC) as the main form of carbon loss in the alkaline soils. Moreover, DIC loss increased with re-occuring EPEs in the soil with the highest pH due to increased dissolution of soil carbonates and elevated contribution of dissolved CO2 from organic carbon degradation (indicated by DIC-δ13C). These results highlight that leaching loss of soil carbon (particularly DIC) is important in the regional carbon budget of arid and semiarid grasslands. With a projected increase of EPEs under climate change, soil carbon leaching processes and its influencing factors warrant better understanding and should be incorporated into soil carbon models when estimating carbon balance in grassland ecosystems.

Low-Level Nitrogen and Short-Term Addition Increase Soil Carbon Sequestration in Chinese Forest Ecosystems

2021 ◽  
Author(s):  
Mbezele Junior Yannick NGABA ◽  
Yves Uwiragiye ◽  
Roland Bol ◽  
Wim de Vries ◽  
Jianbin Zhou
Keyword(s):  
Carbon Sequestration ◽  
Soil Carbon ◽  
Forest Ecosystems ◽  
Soil Carbon Sequestration ◽  
Short Term ◽  
Low Level

scholarly journals Microbial responses to warming enhance soil carbon loss following translocation across a tropical forest elevation gradient

2019 ◽  
Vol 22 (11) ◽  
pp. 1889-1899 ◽  
Author(s):  
Andrew T. Nottingham ◽  
Jeanette Whitaker ◽  
Nick J. Ostle ◽  
Richard D. Bardgett ◽  
Niall P. McNamara ◽  
...  
Keyword(s):  
Tropical Forest ◽  
Soil Carbon ◽  
Elevation Gradient ◽  
Carbon Loss ◽  
Microbial Responses
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