Predicting forested wetland soil carbon using quantitative color sensor measurements in the region of northern Virginia, USA

2021 ◽  
Vol 300 ◽  
pp. 113823
Author(s):  
Stephanie A. Schmidt ◽  
Changwoo Ahn
2020 ◽  
Vol 12 (24) ◽  
pp. 10284
Author(s):  
Xiaoyan Bu ◽  
Dan Cui ◽  
Suocheng Dong ◽  
Wenbao Mi ◽  
Yu Li ◽  
...  

The long-term use of wetlands stresses wetland ecosystems and leads to degradation and C loss. This study explored an optimal remote sensing-multivariate linear regression model (RS-MLRM) for estimating wetland soil organic carbon (SOC) by using a combination of the measured SOC and above ground biomass (AGB) from 273 samples, textural features, spectral information, and a vegetation index calculated from Landsat-8 images using the Ningxia Basin of the Yellow River as the study area. To derive the optimal predictor model for SOC, these variables were regressed against the measured SOC. These were used to predict SOC and evaluate the contribution of wetland restoration and conservation projects to soil carbon sequestration and sinks on the Ningxia Basin of the Yellow River in early (2000 and 2005), intermediate (2010), and recent (2015) years. The results show that from 2000 to 2015, the project-induced contribution to C sequestration was 20.49 TC, with an annual sink of 1.37 TC. This accounted for 54.06% of the total wetland ecosystem C sequestration on the Ningxia Basin of the Yellow River. Moreover, there was a significant success of restoration and conservation projects regarding C sequestration. These restoration and conservation projects have substantially contributed to CO2 mitigation in the arid area.


2019 ◽  
Vol 15 (1) ◽  
pp. 20180407 ◽  
Author(s):  
Samantha K. Chapman ◽  
Matthew A. Hayes ◽  
Brendan Kelly ◽  
J. Adam Langley

Soil oxygen availability may influence blue carbon, which is carbon stored in coastal wetlands, by controlling the decomposition of soil organic matter. We are beginning to quantify soil oxygen availability in wetlands, but we lack a precise understanding of how oxygen controls soil carbon dynamics. In this paper, we synthesize existing data from oxic and anoxic wetland soil incubations to determine how oxygen controls carbon mineralization. We define the oxygen sensitivity of carbon mineralization as the ratio of carbon mineralization rate in oxic soil to this rate in anoxic soil, such that higher values of this ratio indicate greater sensitivity of carbon mineralization to oxygen. The estimates of oxygen sensitivity we derived from existing literature show a wide range of ratios, from 0.8 to 33, across wetlands. We then report oxygen sensitivities from an experimental mesocosm we developed to manipulate soil oxygen status in realistic soils. The variation in oxygen sensitivity we uncover from this systematic review and experiment indicates that Earth system models may misrepresent the oxygen sensitivity of carbon mineralization, and how it varies with context, in wetland soils. We suggest that altered soil oxygen availability could be an important driver of future blue carbon storage in coastal wetlands.


2017 ◽  
Vol 133 (2) ◽  
pp. 165-179 ◽  
Author(s):  
Jason B. Fellman ◽  
David V. D’Amore ◽  
Eran Hood ◽  
Pat Cunningham

Author(s):  
Sergio Zamora ◽  
Luis Carlos Sandoval-Herazo ◽  
Gastón Ballut-Dajud ◽  
Oscar Andrés Del Ángel-Coronel ◽  
Erick Arturo Betanzo-Torres ◽  
...  

Wetland soils are important stores of soil carbon (C) in the biosphere, and play an important role in global carbon cycles in the response strategy to climate change. However, there areknowledge gaps in our understanding of the quantity and distribution in tropical regions. Specifically, Mexican wetlands have not been considered in global carbon budgets or carbon balances for a number of reasons, such as: (1) the lack of data, (2) Spanish publications have not been selected, or (3) because such balances are mainly made in the English language. This study analyzes the literature regarding carbon stocks, sequestration and fluxes in Mexican forested wetlands (Forest-W). Soil carbon stocks of 8, 24.5 and 40.1 kg cm−2 were detected for flooded palms, mangroves, and freshwater or swamps (FW) wetland soils, respectively, indicating that FW soils are the Forest-W with more potential for carbon sinks (p = 0.023), compared to mangroves and flooded palm soils. While these assessments of carbon sequestration were ranged from 36 to 920 g-C m−2 year−1, C emitted as methane was also tabulated (0.6–196 g-C m−2 year−1). Subtracting the C emitted of the C sequestered, 318.2 g-C m−2 year−1 were obtained. Such data revealed that Forest-W function is mainly as carbon sink, and not C source. This review can help to inform practitioners in future decisions regarding sustainable projects, restoration, conservation or creation of wetlands. Finally, it is concluded that Forest-W could be key ecosystems in strategies addressing the mitigation of climate change through carbon storage. However, new studies in this research line and public policies that protect these essential carbon sinks are necessary in order to, hopefully, elaborate global models to make more accurate predictions about future climate.


CATENA ◽  
2020 ◽  
Vol 193 ◽  
pp. 104618 ◽  
Author(s):  
Shuhong Liu ◽  
Fanlong Kong ◽  
Yue Li ◽  
Zhixiang Jiang ◽  
Min Xi ◽  
...  

2018 ◽  
Vol 8 (1) ◽  
Author(s):  
James R. Holmquist ◽  
Lisamarie Windham-Myers ◽  
Norman Bliss ◽  
Stephen Crooks ◽  
James T. Morris ◽  
...  

2018 ◽  
Vol 8 (1) ◽  
Author(s):  
James R. Holmquist ◽  
Lisamarie Windham-Myers ◽  
Norman Bliss ◽  
Stephen Crooks ◽  
James T. Morris ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document