Journal of Geographical Sciences, Volume. 30, Issue 6, 921(2020)

Effects of land use and cultivation time on soil organic and inorganic carbon storage in deep soils

Xia YU1,2,3, Weijian ZHOU1,2,4,5、*, Yunqiang WANG1,4,5,7, Peng CHENG1,2,6,7, Yaoyao HOU1,2, Xiaohu XIONG1,2, Hua DU1,2, Ling YANG1,2,3, and Ya WANG1,2,3
Author Affiliations
  • 1. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, CAS, Xi’an 710061, China
  • 2. Shaanxi Key Laboratory of Accelerator Mass Spectrometry Technology and Application, Xi’an AMS Center, Xi’an 710061, China
  • 3. University of Chinese Academy of Sciences, Beijing 100049, China
  • 4. Interdisciplinary Research Center of Earth Science Frontier, Beijing Normal University, Beijing 100875, China
  • 5. CAS Center for Excellence in Quaternary Science and Global Change, Xi’an 710061, China
  • 6. Open Studio for Oceanic-Continental Climate and Environment Changes, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, Shandong, China
  • 7. Institute of Global Environmental Change, Xi’an Jiaotong University, Xi’an 710049, China
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    Figures & Tables(11)
    Location of the study area and sampling points (n=21 profiles) under different land use types within the Gutun watershed. Cropland includes five restoration time frames: RC-5 (light blue star), RC-15 (light green star), RC-35 (yellow star), RC-60 (red star), RC-70 (black star).
    Vertical distribution of SOC and SIC along 500-cm deep soil profiles. (a) SOC content (open blue circles), means (closed red circles), and the coefficient of variations (green squares); (b) SIC content (open light grey circles), means (closed black circles), and the coefficient of variations (dark red squares)
    Percentage of SOC and SIC stocks in 0-500-cm soil profiles for five land-use types
    Spatial distribution of soil organic carbon stocks (a) and soil inorganic carbon stocks (b) in Gutun watershed
    Soil carbon stocks. (a) SOC stock; (c) SIC stock. (b) and (d) showed the percentage within the bars are proportions of stocks in a 100-cm thick layer compared to the upper 100 cm. Blue circles represent the ratio of the carbon stocks in a given 100-cm layer to the 0-500 cm complete profile. Different lowercase letters indicate significant differences among land uses (p < 0.05), while uppercase letters indicate significant differences among different soil layers within the same land-use type (p < 0.05).
    Changes in carbon stocks with time at different sub-layers: (a) SOC stocks, (b) SIC stocks, and (c) TC stocks at 100-cm intervals
    Changes in SOC, SIC, and TC stocks with time in 0-500 cm soil profiles
    • Table 1.

      Soil properties under five land-use types in the Gutun watershed on the Chinese Loess Plateau

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      Table 1.

      Soil properties under five land-use types in the Gutun watershed on the Chinese Loess Plateau

      Land-use typeTexture (%)BD*(g cm-3)SWC(g kg-1)SOC(g kg-1)SIC(g kg-1)
      SandSiltClay
      Grassland19.2±3.8ab78.2±3.6a2.6±0.3bc1.3±0.1b126.0±20.3b2.96±2.22a16.77±3.00a
      Shrubland19.7±3.0ab77.6±2.8a2.7±0.4bc1.3±0.1b92.8±47.5c2.76±1.75ab13.79±2.40bc
      Forestland22.3±4.5a75.4±4.3a2.3±0.4c1.3±0.1b71.7±19.4c2.58±1.22ab14.82±1.81ab
      Cropland22.1±5.4a75.1±5.0a2.8±0.7b1.5±0.2ab177.2±51.6a2.04±1.10ab12.38±3.18c
      Gully land18.6±4.2b78.2±3.8a3.2±0.6a1.4±0.1a197.7±31.0a1.84±1.29b14.22±2.65bc
    • Table 2.

      Two-way ANOVA* F and p-values for land-use type, cultivation time, and soil depth effects on soil BD (g cm-3), SWC (g kg-1), SOC content (g kg-1), SIC content (g kg-1), SOC stocks (kg m-2), and SIC stocks (kg m-2) in Gutun watershed

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      Table 2.

      Two-way ANOVA* F and p-values for land-use type, cultivation time, and soil depth effects on soil BD (g cm-3), SWC (g kg-1), SOC content (g kg-1), SIC content (g kg-1), SOC stocks (kg m-2), and SIC stocks (kg m-2) in Gutun watershed

      Factor of variationBDSWCSOCSICSOCSSICS
      FpFpFpFpFpFp
      Land-use types24.320.00079.0600.00011.8520.00025.3200.0003.4520.0096.2220.000
      Soil depth2.3100.0336.0800.0004.4340.0002.1210.0004.6510.00017.7810.000
      Time112.590.00036.2830.00018.0820.00031.6660.00021.8670.00013.3650.000
    • Table 3.

      Vertical distribution of SOC and SIC contents (g kg-1) under five land-use types

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      Table 3.

      Vertical distribution of SOC and SIC contents (g kg-1) under five land-use types

      Depth (cm)0-2020-6060-100100-200200-300300-400400-500
      SOCGrassland7.26±4.56aA3.93±3.05aAB2.38±0.93aB2.51±1.12aB3.09±1.68aB2.27±0.61aB1.88±1.35bB
      Shrubland3.79±1.52abA1.55±0.8aB1.07±0.2aB2.89±2.71aA2.71±1.25abA1.77±0.58aB4.40±1.33aA
      Forestland3.29±0.94abA2.90±1.57aA2.38±1.49aA2.08±0.89aA2.39±0.84abA3.19±1.61aA2.03±0.51bA
      Cropland2.52±1.25bA1.81±1.25aAB1.46±0.63aB1.99±1.05aAB1.89±0.86bAB2.34±1.07aAB2.22±1.30bAB
      Gully land1.68±1.27bA1.61±1.14aA2.03±1.57aA2.26±1.77aA1.42±0.39bA
      SICGrassland14.97±1.39abB17.2±2.0abAB17.4±2.2abAB16.25±0.92aB14.18±1.86aB17.45±3.7aAB20.18±2.58aA
      Shrubland16.91±0.01aA16.55±0.21aA16.45±0.07aA14.3±2.9abAB13.31±1.13aB13.21±1.01bB10.96±1.44bB
      Forestland14.27±1.37abA13.97±1.96abA14.42±1.61abA14.75±1.12abA14.57±1.20aA14.76±2.63aA17.01±0.53abA
      Cropland13.40±1.61bA13.39±1.44bA13.05±2.77bA12.68±1.69bA11.99±3.47aA11.52±4.16bA11.34±5.04bA
      Gully land15.10±1.40abA15.66±1.72abA14.91±1.07abA14.17±2.86abA11.88±3.68aA
    • Table 4.

      Vertical distribution of SOC and SIC contents (g kg-1) from RC5 to RC70 croplands in Gutun watershed

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      Table 4.

      Vertical distribution of SOC and SIC contents (g kg-1) from RC5 to RC70 croplands in Gutun watershed

      Depth (cm)0-2020-6060-100100-200200-300300-400400-500
      SOCRC52.02±1aAB1.41±0.94bB1.63±0.78aAB2.35±0.96abAB1.87±0.35bcAB2.96±0.48abA2.6±0.77aAB
      RC151.82±0.5bA1.51±1.82bA1.13±0.66aA1.45±0.88bA1.3±0.89cA1±0.76cA0.72±0.53bA
      RC353.3±0.83aA2.4±1.07aAB1.69±0.26aB2.12±0.43abAB2.34±0.53abAB2.49±0.43abAB2.9±1.5aAB
      RC602.61±1.96aA1.61±1.14bA1.4±0.75aA1.69±0.45bA1.79±0.6cA2.35±1.28bA2.03±1.31abA
      RC703.04±1.18aAB2.26±1.25aAB1.50±0.57aB2.66±1.90aAB3.03±1.02aAB3.45±0.77aA
      SICRC511.95±1.41bA12.47±2.5aA12.66±2.9abA12.29±1.67bA13.56±1.45aA12.9±1.64aA12.75±2.99aA
      RC1514.07±2.21abA14.29±1.2aA14.31±1.11aA12.83±1bAB10.46±5.41aAB6.16±5.2bBC0.94±0.63bC
      RC3513.64±0.37abA13.44±0.73aA14.39±1.09aA13.5±0.51bA13.12±1aA12.99±1.82aA14.13±3.16aA
      RC6014.65±1.39aA13.52±0.93aAB13.32±0.83abAB13.17±0.94bAB12.33±0.9aB13.26±1.93aAB12.9±1.26aAB
      RC7012.35±0.25abA13.13±0.82aA9.65±5.08bA16.43±3.24aA10.53±3.87aA13.09±1.48aA
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    Xia YU, Weijian ZHOU, Yunqiang WANG, Peng CHENG, Yaoyao HOU, Xiaohu XIONG, Hua DU, Ling YANG, Ya WANG. Effects of land use and cultivation time on soil organic and inorganic carbon storage in deep soils[J]. Journal of Geographical Sciences, 2020, 30(6): 921

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    Paper Information

    Received: Sep. 20, 2019

    Accepted: Mar. 5, 2020

    Published Online: Sep. 30, 2020

    The Author Email: Weijian ZHOU (weijian@loess.llqg.ac.cn)

    DOI:10.1007/s11442-020-1762-3

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