scholarly journals Soil carbon stock in fertilized forest stands with mineral soils

2021 ◽  
Author(s):  
Ilze Karklina ◽  
◽  
Andis Lazdins ◽  
Jelena Stola ◽  
Aldis Butlers ◽  
...  

Forest mineral soil is one of the terrestrial carbon pools, and changes in forest management practices can affect the carbon stock in forest soil. The purpose of the study is to estimate temporal fertilization impact on mineral soil organic carbon stock, depending on fertilizers applied, forest stand type, different dominant tree species of the stands. Coniferous and birch forest stands with mineral soil in the central and eastern part of Latvia were selected for the experiment. The fertilizers used were wood ash and nitrogen containing mineral fertilizer. No significant differences in organic carbon stock in O horizon were detected 2–5 years after fertilization. A tendency of smaller organic carbon stock in upper mineral soil layers (0–10 cm, 10–20 cm) was found in most part of objects. Significantly smaller organic carbon stock was found in upper mineral soil layers (0–10 cm and 10–20 cm) in birch stands with wet mineral soil treated with ammonium nitrate if compared to the control plots, possibly due to a different soil moisture regime of forest stands. The positive and significant correlations between soil organic carbon and nitrogen stocks were found in most part of the objects.

2017 ◽  
Vol 40 (2) ◽  
pp. 117-120
Author(s):  
R.K. Verma ◽  
◽  
K.S. Kapoor ◽  

A study was conducted to estimate the biomass and soil carbon stock in various sites of Abies pindrow (Silver fir) - Picea smithiana (Spruce) and Betula utilis (Bhojpatra) forests of district Shimla, Himachal Pradesh during the year 2014-2015. In Fir-Spruce mixed forests, the amount of carbon stock at Larot site for above ground, below ground, under storey and litter was 287.39 tC/ha, 57.48 tC/ha, 2.22 tC/ha and 0.92 tC/ha respectively. Whereas, values of these components at Khirki site were 267.31 tC/ha, 53.46 tC/ha, 3.65 tC/ha and 0.85 tC/ha respectively. The biomass as well as the carbon stock was higher at Larot site than Khirki site. The soil organic carbon stock (tC/ha) at 10-15 cm, 15-30 cm and 30-45 cm was 27.05, 24.91 and 18.35 respectively at Larot site. Whereas, these values for different depths were 27.36 tC/ha, 22.02 tC/ha and 19.01 tC/ha respectively for Khirki site. The value of total soil carbon stock was little more (70.31 tC/ha) at Larot site than Khirki site (68.39 tC/ha). In case of Bhojpatra forests, the amount of carbon stock at Larot site for above ground, below ground, under storey and litter was 75.32 tC/ha, 18.83 tC/ha, 11.38 tC/ha and 1.57 tC/ha respectively. In Bhojpatra forests, understorey i.e. biomass of shrubs and herbs contribute about 11.63% to the total biomass in the forest. The soil organic carbon stock (tC/ha) at 10-15 cm, 15-30 cm and 30-45 cm was 19.54, 15.43 and 11.88 respectively for this site. The soil organic carbon stock decreased with increasing the soil depth.


2020 ◽  
Vol 56 (1) ◽  
pp. 128-136
Author(s):  
Paulo Henrique Marques Monroe ◽  
Patrícia Anjos Bittencourt Barreto-Garcia ◽  
Maida Cynthia Duca Lima ◽  
Rayka Kristian Alves Santos ◽  
Elismar Pereira Oliveira ◽  
...  

The objective of this work was to evaluate the distribution of fine roots and its influence on the soil organic carbon stock, at a depth of 20 cm, in a Grevillea robusta and Coffea arabica agroforestry system. The study was conducted in an agroforestry system established 15 years ago in a transition area of Caatinga and Atlantic Forest biomes in Brazil. G. robusta trees representing the most frequent diameter class were selected, and three distances of these trees (0, 0.75 and 1.50 m) and two soil collection depths (0–10 and 10–20 cm) were defined. The root samples were scanned and quantified using a software program. There was a general predominance of roots with a diameter of 0.6 mm at the shortest distance from the surface layer, while there was a predominance of roots with a diameter of 0.4 mm in the 10–20 cm layer. The root carbon stock at a distance of 0.75 m was higher at a depth of 0–10 cm (0.60 Mg ha-1). The soil organic carbon stock also showed higher results in the 0–10 cm layer compared to the 10–20 cm layer, although with significant variation only in the distance of 1.5 m. There was a higher concentration of fine roots in the topsoil, probably influenced by a greater availability of water and nutrients from plant residues. The soil carbon stock is not closely related to root density or root carbon stock. The data presented in this study do not provide a definitive conclusion.


CATENA ◽  
2018 ◽  
Vol 160 ◽  
pp. 76-89 ◽  
Author(s):  
Zhao Chen ◽  
Jing Wang ◽  
Nanrong Deng ◽  
Changhe Lv ◽  
Qi Wang ◽  
...  

Forests ◽  
2021 ◽  
Vol 12 (4) ◽  
pp. 394
Author(s):  
Xinhui Xu ◽  
Zhenkai Sun ◽  
Zezhou Hao ◽  
Qi Bian ◽  
Kaiyue Wei ◽  
...  

Forests can affect soil organic carbon (SOC) quality and distribution through forest types and traits. However, much less is known about the influence of urban forests on SOC, especially in the effects of different forest types, such as coniferous and broadleaved forests. Our objectives were to assess the effects of urban forest types on the variability of SOC content (SOC concentration (SOCC) and SOC density (SOCD)) and determine the key forest traits influencing SOC. Data from 168 urban forest plots of coniferous or broadleaved forests located in the Beijing urban area were used to predict the effects of forest types and traits on SOC in three different soil layers, 0–10 cm, 10–20 cm, and 20–30 cm. The analysis of variance and multiple comparisons were used to test the differences in SOC between forest types or layers. Partial least squares regression (PLSR) was used to explain the influence of forest traits on SOC and select the significant predictors. Our results showed that in urban forests, the SOCC and SOCD values of the coniferous forest group were both significantly higher than those of the broadleaved group. The SOCC of the surface soil was significantly higher than those of the following two deep layers. In PLSR models, 42.07% of the SOCC variance and 35.83% of the SOCD variance were explained by forest traits. Diameter at breast height was selected as the best predictor variable by comparing variable importance in projection (VIP) scores in the models. The results suggest that forest types and traits could be used as an optional approach to assess the organic carbon stock in urban forest soils. This study found substantial effects of urban forest types and traits on soil organic carbon sequestration, which provides important data support for urban forest planning and management.


2013 ◽  
Vol 10 (5) ◽  
pp. 866-872 ◽  
Author(s):  
Xiao-guo Wang ◽  
Bo Zhu ◽  
Ke-ke Hua ◽  
Yong Luo ◽  
Jian Zhang ◽  
...  

2019 ◽  
Vol 23 (1) ◽  
pp. 159-171 ◽  
Author(s):  
Claudia Canedoli ◽  
Chiara Ferrè ◽  
Davide Abu El Khair ◽  
Emilio Padoa-Schioppa ◽  
Roberto Comolli

2017 ◽  
Vol 39 (2) ◽  
pp. 169 ◽  
Author(s):  
Heyun Wang ◽  
Zhi Dong ◽  
Jianying Guo ◽  
Hongli Li ◽  
Jinrong Li ◽  
...  

Grassland ecosystems, an important component of the terrestrial environment, play an essential role in the global carbon cycle and balance. We considered four different grazing intensities on a Stipa breviflora desert steppe: heavy grazing (HG), moderate grazing (MG), light grazing (LG), and an area fenced to exclude livestock grazing as the Control (CK). The analyses of the aboveground biomass, litter, belowground biomass, soil organic carbon and soil light fraction organic carbon were utilised to study the organic carbon stock characteristics in the S. breviflora desert steppe under different grazing intensities. This is important to reveal the mechanisms of grazing impact on carbon processes in the desert steppe, and can provide a theoretical basis for conservation and utilisation of grassland resources. Results showed that the carbon stock was 11.98–44.51 g m–2 in aboveground biomass, 10.43–36.12 g m–2 in plant litters, and 502.30–804.31 g m–2 in belowground biomass (0–40 cm). It was significantly higher in CK than in MG and HG. The carbon stock at 0–40-cm soil depth was 7817.43–9694.16 g m–2, and it was significantly higher in LG than in CK and HG. The total carbon stock in the vegetation-soil system was 8342.14–10494.80 g m–2 under different grazing intensities, with the largest value in LG, followed by MG, CK, and HG. About 90.54–93.71% of the total carbon in grassland ecosystem was reserved in soil. The LG and MG intensities were beneficial to the accumulation of soil organic carbon stock. The soil light fraction organic carbon stock was 484.20–654.62 g m–2 and was the highest under LG intensity. The LG and MG intensities were beneficial for soil nutrient accumulation in the desert steppe.


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