Calculating Organic Carbon Stock from Forest Soils

被引:25
作者
Dinca, Lucian Constantin [1 ]
Dinca, Maria [1 ]
Vasile, Diana [1 ]
Sparchez, Gheorghe [2 ]
Holonec, Liviu [3 ]
机构
[1] Natl Forest Res Dev Inst Marin Dracea, Brasov 500035, Romania
[2] Transilvania Univ Brasov, Fac Silviculture & Forest Engn, Brasov 500123, Romania
[3] Univ Agr Sci & Vet Med, Cluj Napoca 400372, Romania
关键词
carbon stocks; organic carbon; pedogenetical horizons; soil types; standard depth; LAND-USE CHANGE; SPATIAL-PATTERNS; SLOPE GRADIENT; SEQUESTRATION; STORAGE; UNCERTAINTY; ECOSYSTEMS; DYNAMICS; EUROPE; MATTER;
D O I
10.15835/nbha43210141
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
The organic carbon stock (SOC) (t/ha) was calculated in different approaches in order to enhance the differences among methods and their utility regarding specific studies. Using data obtained in Romania (2000-2012) from 4,500 profiles and 9,523 soil horizons, the organic carbon stock was calculated for the main forest soils (18 types) using three different methods: 1) on pedogenetical horizons, by soil bulk density and depth class/horizon thickness; 2) by soil type and standard depths; 3) using regression equations between the quantity of organic C and harvesting depths. Even though the same data were used, the differences between the values of C stock obtained from the three methods were relatively high. The first method led to an overvaluation of the C stock. The differences between methods I and 2 were high (and reached 33% for andosol), while the differences between methods 2 and 3 were smaller (a maximum of 23% for rendzic leptosol). The differences between methods 2 and 3 were significantly lower especially for andosol, arenosol and vertisol. A thorough analysis of all three methods concluded that the best method to evaluate the organic C stock was to distribute the obtained values on the following standard depths: 0 - 10 cm; 10 - 20 cm; 20 - 40 an; > 40 cm. For each soil type, a correlation between the quantity of organic C and the sample harvesting depth was also established. These correlations were significant for all types of soil; however, lower correlation coefficients were registered for rendzic leptosol, haplicpodzol and fluvisol.
引用
收藏
页码:568 / 575
页数:8
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