scholarly journals Verifiable soil organic carbon modelling to facilitate regional reporting of cropland carbon change: A test case in the Czech Republic

2020 ◽  
Vol 274 ◽  
pp. 111206
Author(s):  
Juraj Balkovič ◽  
Mikuláš Madaras ◽  
Rastislav Skalský ◽  
Christian Folberth ◽  
Michaela Smatanová ◽  
...  
2020 ◽  
Author(s):  
Asa Gholizadeh ◽  
Raphael Viscarra Rossel ◽  
Mohammadmehdi Saberioon ◽  
Lubos Boruvka ◽  
Lenka Pavlu

<p>Any strategy to change Carbon (C) pool would have a substantial effect on functionality of numerous ecosystem functions, detachment of Soil Organic Carbon (SOC), atmospheric carbon dioxide (CO<sub>2</sub>) concentration, and climate change mitigation. As the largest amount of the world’s C is stored in forests soils, the importance of forest SOC management is highlighted. Total SOC in forest varies not only laterally but also vertically with depth; however, the SOC storage of lower soil horizons have not been investigated enough despite their potential to frame our understanding of soil functioning. Visible–Near Infrared (vis–NIR) reflectance spectroscopy enables rapid examinations of the horizontal distribution of forest SOC, overcoming limitations of traditional soil assessment. This study aims to evaluate the potential of vis–NIR spectroscopy for characterizing the SOC contents of organic and mineral horizons in forests. We investigated 1080 forested sites across the Czech Republic at five individual soil layers, representing the Litter (L), Fragmented (F), and Humus (H) organic horizons, and the A<sub>1</sub> (depth of 2–10 cm) and A<sub>2</sub> (depth of 10–40 cm) mineral horizons (total 5400 samples). We then used Support Vector Machine (SVM) to model the SOC contents of (i) the profile (all organic and mineral horizons together), (ii) the combined organic horizons, (iii) the combined mineral horizons, and (iv) each individual horizon separately. The models were validated using 10-repeated 10-fold cross validation. Results showed that there was at least more than seven times as much SOC in the combined organic horizons compared to the combined mineral horizons with more variation in deeper layers. All individual horizons’ SOC was successfully predicted with low error and R<sup>2</sup> values higher than 0.63; however, the prediction accuracy of F and A<sub>1</sub> was greater compared to others (R<sup>2</sup> > 0.70 and very low-biased spatial estimates). We have shown that modelling of SOC with vis–NIR spectra in different soil horizons of highly heterogeneous forests of the Czech Republic is practical.</p>


Geoderma ◽  
2021 ◽  
Vol 385 ◽  
pp. 114832
Author(s):  
Asa Gholizadeh ◽  
Raphael A. Viscarra Rossel ◽  
Mohammadmehdi Saberioon ◽  
Luboš Borůvka ◽  
Josef Kratina ◽  
...  

2021 ◽  
Vol 13 (12) ◽  
pp. 2265
Author(s):  
Jonathan Sanderman ◽  
Kathleen Savage ◽  
Shree Dangal ◽  
Gabriel Duran ◽  
Charlotte Rivard ◽  
...  

A major limitation to building credible soil carbon sequestration programs is the cost of measuring soil carbon change. Diffuse reflectance spectroscopy (DRS) is considered a viable low-cost alternative to traditional laboratory analysis of soil organic carbon (SOC). While numerous studies have shown that DRS can produce accurate and precise estimates of SOC across landscapes, whether DRS can detect subtle management induced changes in SOC at a given site has not been resolved. Here, we leverage archived soil samples from seven long-term research trials in the U.S. to test this question using mid infrared (MIR) spectroscopy coupled with the USDA-NRCS Kellogg Soil Survey Laboratory MIR spectral library. Overall, MIR-based estimates of SOC%, with samples scanned on a secondary instrument, were excellent with the root mean square error ranging from 0.10 to 0.33% across the seven sites. In all but two instances, the same statistically significant (p < 0.10) management effect was found using both the lab-based SOC% and MIR estimated SOC% data. Despite some additional uncertainty, primarily in the form of bias, these results suggest that large existing MIR spectral libraries can be operationalized in other laboratories for successful carbon monitoring.


Eos ◽  
2010 ◽  
Vol 91 (47) ◽  
pp. 441 ◽  
Author(s):  
David J. Brown ◽  
E. Raymond Hunt ◽  
R. César Izaurralde ◽  
Keith H. Paustian ◽  
Charles W. Rice ◽  
...  

2011 ◽  
Vol 47 (7) ◽  
pp. 745-752 ◽  
Author(s):  
Minggang Xu ◽  
Yilai Lou ◽  
Xiaolin Sun ◽  
Wei Wang ◽  
Muhammad Baniyamuddin ◽  
...  

2006 ◽  
Vol 52 (5) ◽  
pp. 495-505 ◽  
Author(s):  
Jaromír Kubát ◽  
Dana Cerhanová ◽  
Jitka Nováková ◽  
Jan Lipavský

2012 ◽  
Vol 82-83 ◽  
pp. 115-128 ◽  
Author(s):  
Yongqiang Yu ◽  
Yao Huang ◽  
Wen Zhang

2014 ◽  
Vol 1073-1076 ◽  
pp. 632-637
Author(s):  
Xue Mei Li ◽  
Guang Ju Hao

Soil carbon pool is an important component of the ecosystem carbon pools. It plays a key role in mitigating the global warming and control the concentration of greenhouse gas. The areas of urban land have changed dramatically both in quality and quantity due to the land-based urbanization and industrialization. This paper analyzed the change of the soil organic carbon reserves under the land use change in Tianjin Binhai New Area (TBNA) from 1995 to 2012. The results showed that the land use change was one of the important reasons of the soil organic carbon change, and the soil organic carbon reserves of land use change in TBNA was reduced from3.339mt (million ton) to 5.842mt in this stage.


Sign in / Sign up

Export Citation Format

Share Document