[논문]Cations of Soil Minerals and Carbon Stabilization of Three Land Use Types in Gambari Forest Reserve, Nigeria

Falade, Oladele Fisayo; Rufai, Samsideen Olabiyi

doi:10.7747/jfes.2021.37.2.116

[국내논문] Cations of Soil Minerals and Carbon Stabilization of Three Land Use Types in Gambari Forest Reserve, Nigeria 원문보기

Journal of forest and environmental science, v.37 no.2, 2021년, pp.116 - 127

Falade, Oladele Fisayo (Department of Forest Production and Products, University of Ibadan) , Rufai, Samsideen Olabiyi (Forestry Research Institute of Nigeria)

Abstract ▼ AI-Helper

Predicting carbon distribution of soil aggregates is difficult due to complexity in organo-mineral formation. This limits global warming mitigation through soil carbon sequestration. Therefore, knowledge of land use effect on carbon stabilization requires quantification of soil mineral cations. The study was conducted to quantify carbon and base cations on soil mineral fractions in Natural Forest, Plantation Forest and Farm Land. Five 0.09 ha were demarcated alternately along 500 m long transect with an interval of 50 m in Natural Forest (NF), Plantation Forest (PF) and Farm Land (FL). Soil samples were collected with soil cores at 0-15, 15-30 and 30-45 cm depths in each plot. Soil core samples were oven-dried at 105℃ and soil bulk densities were computed. Sample (100 g) of each soil core was separated into >2.0, 2.0-1.0, 1.0-0.5, 0.5-0.05 and <0.05 mm aggregates using dry sieve procedure and proportion determined. Carbon concentration of soil aggregates was determined using Loss-on-ignition method. Mineral fractions of soil depths were obtained using dispersion, sequential extraction and sedimentation methods of composite soil samples and sieved into 0.05 mm fractions. Cation exchange capacity of two mineral fractions was measured using spectrophotometry method. Data collected were analysed using descriptive and ANOVA at α0.05. Silt and sand particle size decreased while clay increased with increase in soil depth in NF and PF. Subsoil depth contained highest carbon stock in the PF. Carbon concentration increased with decrease in aggregate size in soil depths of NF and FL. Micro- (1-0.5, 0.5-0.05 and 2.0 and 2-1.0 mm) were saturated with soil carbon in NF and FL, respectively. Cation exchange capacity of 0.05 mm in soil depths of PF and FL. Fine silt (<0.05 mm) determine the cation exchange capacity in soil depths. Land use and mineral size influence the carbon and cation exchange capacity of Gambari Forest Reserve.

주제어

표/그림 (8)

그림 Fig. 1. Map of the study area.
표 Table 1. Particle size of soil depths in Natural Forest, Plantation Forest and Farm Land in Gambari Forest Reserve
표 Table 2. Soil carbon concentration of Natural Forest, Plantation Forest and Farm Land of Gambari Forest Reserve
표 Table 3. Soil carbon stock of Natural Forest, Plantation Forest and Farm Land in Gambari Forest Reserve
그림 Fig. 2. (A) Organic carbon of aggregate sizes in the soil depths of Natural Forest, (B) organic carbon of aggregate sizes in soil depths of Plantation Forest, (C) organic carbon of aggregate sizes in the soil depths of Farm Land.
$Table 4. Cation exchange capacity of two soil mineral fractions in three depths of Natural Forest$ 표 Table 4. Cation exchange capacity of two soil mineral fractions in three depths of Natural Forest
표 Table 5. Cation exchangeable capacity of soil mineral particles at three depths of Plantation Forest
표 Table 6. Cation exchangeable capacity of soil mineral particles at three depths of Farm Land

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