Spatial Variation of Organic Carbon Stocks in Peat Soils and Gleyzems in the Northeast of Sakhalin Island

被引:5
|
作者
Lipatov, D. N. [1 ]
Shcheglov, A., I [1 ]
Manakhov, D., V [1 ]
Brekhov, P. T. [2 ]
机构
[1] Lomonosov Moscow State Univ, Moscow 119991, Russia
[2] Voronezh State Agr Univ, Voronezh 394087, Russia
关键词
bog soils; soil profile; sampling; soil monitoring; Fibric Histosols; Histic Gleysols;
D O I
10.1134/S1064229321020083
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Stocks of organic carbon in the northeast of Sakhalin Island average 109.8 kg/m(2) in medium-deep oligotrophic peat soils, 75.8 kg/m(2) in oligotrophic peat gley soils, 20.9-42.7 kg/m(2) in peat gleyzems, and 16.6 kg/m(2) in gleyzems. The vertical distribution of volumetric concentrations and the carbon stocks in different subtypes of peat soils and gleyzems have been studied. Linear regression equations have been developed to estimate carbon stocks in dependence on the depth of the peat layer. The coefficients of variation of the carbon stocks on test plots of 50 x 50 m in size increase in the following order: medium-deep oligotrophic peat soils (3.1-7.3%) < oligotrophic peat gley soils (3.3-12.9%) < peat gleyzems (9.2-21.7%) < gleyzems (22.9%). The proportion of the carbon stock variances has been estimated for three spatial scales (50 x 50 m, 5 x 5 km, and 10 x 10 km) with the use of the hierarchical analysis of variance. The required number of sampled profiles for reliable data on the mean carbon stocks in peat soils and gleyzems has been estimated. Nomograms for determining the least significant difference between the estimates of the mean soil carbon stocks have been proposed for studies with a small number of samples.
引用
收藏
页码:226 / 237
页数:12
相关论文
共 50 条
  • [31] Spatial Heterogeneity in the Properties of High-Moor Peat Soils under Local Pyrogenesis in Northeastern Sakhalin
    D. N. Lipatov
    A. I. Shcheglov
    D. V. Manakhov
    P. T. Brekhov
    Eurasian Soil Science, 2016, 49 : 238 - 250
  • [32] Spatial Heterogeneity in the Properties of High-Moor Peat Soils under Local Pyrogenesis in Northeastern Sakhalin
    Lipatov, D. N.
    Shcheglov, A. I.
    Manakhov, D. V.
    Brekhov, P. T.
    EURASIAN SOIL SCIENCE, 2016, 49 (02) : 238 - 250
  • [33] Carbon Accumulation in Peat Soils of Floodplain Mires in the Northeast of the Central Russian Upland
    Volkova, E. M.
    Leonova, O. A.
    Golovchenko, A. V.
    EURASIAN SOIL SCIENCE, 2024, 57 (03) : 419 - 429
  • [34] Carbon Accumulation in Peat Soils of Floodplain Mires in the Northeast of the Central Russian Upland
    E. M. Volkova
    O. A. Leonova
    A. V. Golovchenko
    Eurasian Soil Science, 2024, 57 : 419 - 429
  • [35] Temporal and spatial changes in soil organic carbon and soil inorganic carbon stocks in the semi-arid area of northeast China
    Wang, Shuai
    Zhuang, Qianlai
    Zhou, Mingyi
    Jin, Xinxin
    Yu, Na
    Yuan, Ting
    ECOLOGICAL INDICATORS, 2023, 146
  • [36] Spatial distribution of soil organic carbon stocks in France
    Martin, M. P.
    Wattenbach, M.
    Smith, P.
    Meersmans, J.
    Jolivet, C.
    Boulonne, L.
    Arrouays, D.
    BIOGEOSCIENCES, 2011, 8 (05) : 1053 - 1065
  • [37] Precise estimation of soil organic carbon stocks in the northeast Tibetan Plateau
    Yang, Ren-Min
    Zhang, Gan-Lin
    Yang, Fei
    Zhi, Jun-Jun
    Yang, Fan
    Liu, Feng
    Zhao, Yu-Guo
    Li, De-Cheng
    SCIENTIFIC REPORTS, 2016, 6
  • [38] The Impact of Permafrost Change on Soil Organic Carbon Stocks in Northeast China
    Song, Yang
    Huang, Shuai
    Zhang, Haiying
    Wang, Qin
    Ding, Lin
    Liu, Yanjie
    Domisch, Timo
    FORESTS, 2024, 15 (01):
  • [39] Precise estimation of soil organic carbon stocks in the northeast Tibetan Plateau
    Ren-Min Yang
    Gan-Lin Zhang
    Fei Yang
    Jun-Jun Zhi
    Fan Yang
    Feng Liu
    Yu-Guo Zhao
    De-Cheng Li
    Scientific Reports, 6
  • [40] Assessment of Organic Carbon Stocks in Forest Soils on a Regional Scale
    Chernova, O. V.
    Ryzhova, I. M.
    Podvezennaya, M. A.
    EURASIAN SOIL SCIENCE, 2020, 53 (03) : 339 - 348