Integrated Approach to Spatial Assessment of Soil Organic Carbon in the Russian Federation

被引:20
作者
Chernova, O., V [1 ]
Golozubov, O. M. [2 ]
Alyabina, I. O. [2 ]
Schepaschenko, D. G. [3 ,4 ]
机构
[1] Russian Acad Sci, Severtsov Inst Ecol & Evolut, Leninskii Pr 33, Moscow 119071, Russia
[2] Lomonosov Moscow State Univ, Moscow 119991, Russia
[3] Int Inst Appl Syst Anal, Schlosspl 1, A-2361 Laxenburg, Austria
[4] Russian Acad Sci, Ctr Forest Ecol & Prod, Profsoyuznaya 84-32,Str 14, Moscow 117997, Russia
关键词
structure of soil carbon stock; bulk density; soil mapping; BULK-DENSITY; PEDOTRANSFER FUNCTIONS; STOCKS; UNCERTAINTY; DYNAMICS; LAND;
D O I
10.1134/S1064229321030042
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
An approach was developed and tested to spatial assessment of soil organic carbon stock in uniform groups of mineral and organic (litters, peat deposits, and peaty horizons of semihydromorphic soils) soil horizons. Estimation algorithm allowed us to utilize various datasets with different scales, both spatially and attributive sparse data of different veracities, which complemented each other. A series of maps of different accuracies and scales, including coarse-scale maps covering the entire country and more detailed maps for regions well covered with field measurements. Using these maps, the total organic carbon amount and its distribution over different pools in the 30-cm topsoil layer for the entire Russia and for three administrative regions of European Russia (more detailed) were estimated. The soil organic carbon pool of mineral soil horizons was estimated at 101 Gt C, which corresponded to 62% of the total organic carbon stock within the layer of 0-30 cm; 38% is allocated in organic horizons, including 9% in litter horizons (in rapidly decomposing organic pool) and 29% in peat deposit and peaty horizons of semihydromorphic soils. The organic carbon stocks in the 30-cm soil layer gradually increase from the north to the south: from 87 t/ha in Vologda oblast to 91 t/ha in Moscow oblast and 109 t/ha in Rostov oblast. The share of organic horizons in the total carbon stock decreases from the north to the south. Information on the size and structure of organic carbon pools may facilitate more reliable assessments of soil tolerance toward natural and anthropogenic changes and the development of regionally specific land use strategies.
引用
收藏
页码:325 / 336
页数:12
相关论文
共 52 条
[1]   Evaluation of pedotransfer functions for predicting soil bulk density for U.S. soils [J].
Abdelbaki, Ahmed M. .
AIN SHAMS ENGINEERING JOURNAL, 2018, 9 (04) :1611-1619
[2]  
Alabina I.O., 2019, SOIL MAP CRIMEA SCAL
[3]  
[Anonymous], 1969, TUNDRA SOILS NO YAKU
[4]   Harmonized soil property values for broad-scale modelling (WISE30sec) with estimates of global soil carbon stocks [J].
Batjes, N. H. .
GEODERMA, 2016, 269 :61-68
[5]  
Bazilevich N.I., 1986, GEOGRAPHIC PATTERN S
[6]  
Bazilevich N. I., 1993, Biological Productivity of Ecosystems of Northern Eurasia
[7]   Pedotransfer functions for estimating soil bulk density from existing soil survey reports in Brazil [J].
Benites, Vinicius M. ;
Machado, Pedro L. O. A. ;
Fidalgo, Elaine C. C. ;
Coelho, Mauricio R. ;
Madari, Beata E. .
GEODERMA, 2007, 139 (1-2) :90-97
[8]  
Berdsi R.A., 1994, CARBON FOREST BOG EC
[9]  
Boschi RS, 2018, SCI AGR, V75, P70, DOI [10.1590/1678-992x-2016-0357, 10.1590/1678-992X-2016-0357]
[10]  
Chaikaew P., 2017, Applied and Environmental Soil Science, V2017, P4010381, DOI [10.1155/2017/4010381, DOI 10.1155/2017/4010381]