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Distribution and Accumulation of Soil Carbon in Temperate Wetland, Northeast China

LYU Mingzhi SHENG Lianxi ZHANG Zhongsheng ZHANG Li

LYU Mingzhi, SHENG Lianxi, ZHANG Zhongsheng, ZHANG Li. Distribution and Accumulation of Soil Carbon in Temperate Wetland, Northeast China[J]. 中国地理科学, 2016, 26(3): 295-303. doi: 10.1007/s11769-016-0809-y
引用本文: LYU Mingzhi, SHENG Lianxi, ZHANG Zhongsheng, ZHANG Li. Distribution and Accumulation of Soil Carbon in Temperate Wetland, Northeast China[J]. 中国地理科学, 2016, 26(3): 295-303. doi: 10.1007/s11769-016-0809-y
LYU Mingzhi, SHENG Lianxi, ZHANG Zhongsheng, ZHANG Li. Distribution and Accumulation of Soil Carbon in Temperate Wetland, Northeast China[J]. Chinese Geographical Science, 2016, 26(3): 295-303. doi: 10.1007/s11769-016-0809-y
Citation: LYU Mingzhi, SHENG Lianxi, ZHANG Zhongsheng, ZHANG Li. Distribution and Accumulation of Soil Carbon in Temperate Wetland, Northeast China[J]. Chinese Geographical Science, 2016, 26(3): 295-303. doi: 10.1007/s11769-016-0809-y

Distribution and Accumulation of Soil Carbon in Temperate Wetland, Northeast China

doi: 10.1007/s11769-016-0809-y
基金项目: Under the auspices of National Natural Science Foundation of China (No. 41471081), Scientific Research Foundation of Graduate School of Northeast Normal University (No. 12SSXT149)
详细信息
    通讯作者:

    SHENG Lianxi

Distribution and Accumulation of Soil Carbon in Temperate Wetland, Northeast China

Funds: Under the auspices of National Natural Science Foundation of China (No. 41471081), Scientific Research Foundation of Graduate School of Northeast Normal University (No. 12SSXT149)
More Information
    Corresponding author: SHENG Lianxi
  • 摘要: Estimating carbon sequestration and nutrient accumulation rates in Northeast China are important to assess wetlands function as carbon sink buffering greenhouse gas increasing in North Asia. The objectives of this study were to estimate accreting rates of carbon and nutrients in typical temperate wetlands. Results indicated that average soil organic carbon (SOC), total nitrogen (TN) and total phosphorus (TP) contents were 37.81%, 1.59% and 0.08% in peatlands, 5.33%, 0.25% and 0.05% in marshes, 2.92%, 0.27% and 0.10% in marshy meadows, respectively. Chronologies reconstructed by 210Pb in the present work were acceptable and reliable, and the average time to yield 0-40 cm depth sediment cores was 150 years. Average carbon sequestration rate (Carbonsq), nitrogen and phosphorus accumulation rates were 219.4 g C/(m2·yr), 9.16 g N/(m2·yr) and 0.46 g P/(m2·yr) for peatland; 57.13 g C/(m2·yr), 5.42 g N/(m2·yr) and 2.16 g P/(m2·yr) for marshy meadow; 78.35 g C/(m2·yr), 8.70 g N/(m2·yr) and 0.71 g P/(m2·yr) for marshy; respectively. Positive relations existed between Carbonsq with nitrogen and precipitations, indicating that Carbonsq might be strengthened in future climate scenarios.
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Distribution and Accumulation of Soil Carbon in Temperate Wetland, Northeast China

doi: 10.1007/s11769-016-0809-y
    基金项目:  Under the auspices of National Natural Science Foundation of China (No. 41471081), Scientific Research Foundation of Graduate School of Northeast Normal University (No. 12SSXT149)
    通讯作者: SHENG Lianxi

摘要: Estimating carbon sequestration and nutrient accumulation rates in Northeast China are important to assess wetlands function as carbon sink buffering greenhouse gas increasing in North Asia. The objectives of this study were to estimate accreting rates of carbon and nutrients in typical temperate wetlands. Results indicated that average soil organic carbon (SOC), total nitrogen (TN) and total phosphorus (TP) contents were 37.81%, 1.59% and 0.08% in peatlands, 5.33%, 0.25% and 0.05% in marshes, 2.92%, 0.27% and 0.10% in marshy meadows, respectively. Chronologies reconstructed by 210Pb in the present work were acceptable and reliable, and the average time to yield 0-40 cm depth sediment cores was 150 years. Average carbon sequestration rate (Carbonsq), nitrogen and phosphorus accumulation rates were 219.4 g C/(m2·yr), 9.16 g N/(m2·yr) and 0.46 g P/(m2·yr) for peatland; 57.13 g C/(m2·yr), 5.42 g N/(m2·yr) and 2.16 g P/(m2·yr) for marshy meadow; 78.35 g C/(m2·yr), 8.70 g N/(m2·yr) and 0.71 g P/(m2·yr) for marshy; respectively. Positive relations existed between Carbonsq with nitrogen and precipitations, indicating that Carbonsq might be strengthened in future climate scenarios.

English Abstract

LYU Mingzhi, SHENG Lianxi, ZHANG Zhongsheng, ZHANG Li. Distribution and Accumulation of Soil Carbon in Temperate Wetland, Northeast China[J]. 中国地理科学, 2016, 26(3): 295-303. doi: 10.1007/s11769-016-0809-y
引用本文: LYU Mingzhi, SHENG Lianxi, ZHANG Zhongsheng, ZHANG Li. Distribution and Accumulation of Soil Carbon in Temperate Wetland, Northeast China[J]. 中国地理科学, 2016, 26(3): 295-303. doi: 10.1007/s11769-016-0809-y
LYU Mingzhi, SHENG Lianxi, ZHANG Zhongsheng, ZHANG Li. Distribution and Accumulation of Soil Carbon in Temperate Wetland, Northeast China[J]. Chinese Geographical Science, 2016, 26(3): 295-303. doi: 10.1007/s11769-016-0809-y
Citation: LYU Mingzhi, SHENG Lianxi, ZHANG Zhongsheng, ZHANG Li. Distribution and Accumulation of Soil Carbon in Temperate Wetland, Northeast China[J]. Chinese Geographical Science, 2016, 26(3): 295-303. doi: 10.1007/s11769-016-0809-y
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