洛阳市农田土壤碳汇规律研究

    Carbon sink in farmland soils in Luoyang City, China

    • 摘要: 依据不同时期洛阳市多目标区域地球化学调查点的重复采样分析数据,研究农田土壤全碳、有机碳的密度、储量空间分布特征、变化规律与影响因素。结果表明,2005年多目标调查区农田表层土壤全碳含量平均值为1.57%,全碳密度平均值为44.74 t/hm2;有机碳含量平均值为1.12%,有机碳密度平均值为34.27 t/hm2;全碳密度平均增长0.709 t/hm2,有机碳密度平均增长6.643 t/hm2;全碳年均增加量41.73 kg/(hm2·a),有机碳年均增加量390.75 kg/(hm2·a);全碳储量1 251.13万t,有机碳储量887.959万t;全碳储量变化量19.828万t,有机碳储量变化量185.78万t,均呈增长特征。2018年多目标调查区农田表层土壤全碳含量平均值为1.18%,全碳密度平均值为34.27 t/hm2;有机碳含量平均值为1.07%,有机碳密度平均值为30.94 t/hm2;全碳密度平均减少9.642 t/hm2,有机碳密度平均增长4.727 t/hm2;全碳年均增加量-2 410.5 kg/(hm2·a),有机碳年均增加量1 181.75 kg/(hm2·a);全碳储量196.35万t,有机碳储量177.261万t;全区农田土壤表层全碳储量为1 447.481万t,有机碳储量为1 065.22万t;全碳储量变化量-55.241万t,呈减少特征,有机碳储量变化量27.082万t,呈增加特征。研究区总体上全碳减少35.413万t,有机碳储量增加212.862万t;全碳与有机碳、CaO、MgO、N、P呈显著正相关,有机碳与全碳、N、P呈显著正相关,pH与CaO呈显著正相关;施肥增加了农田土壤中有机碳和全碳含量,全碳受CaO影响显著;碳酸盐区发育的碱性土壤环境下呈碳汇特征;在南部土壤变酸性环境下,土壤中碳酸盐类分解,形成碳损失和钙减少。该研究成果为洛阳市碳达峰、碳中和研究提供了重要科学依据。

       

      Abstract: This study investigates the spatial distribution characteristics, temporal changes, and influencing factors of total carbon density, organic carbon density, and reserves in the farmland soils in Luoyang City based on repeated sampling data from multi-purpose regional geochemical survey points over different periods. The results indicate that in 2005, the topsoils in the multi-purpose survey area exhibited an average total carbon content of 1.57%, an average total carbon density of 44.74 t/hm2, an average organic carbon content of 1.12%, and an average organic carbon density of 34.27 t/hm2. With annual average increases in the total carbon density and organic carbon density of 0.709 t/hm2 and 6.643 t/hm2, respectively, this year witnessed increases in the total carbon and organic carbon of 41.73 kg/(hm2·a) and 390.75 kg/(hm2·a), respectively. The respective reserves of total carbon and organic carbon were 12.511 3 million tons and 8.879 59 million tons, with respective increases of 198.28 thousand tons and 1.857 8 million tons. In 2018, the topsoils in the multi-purpose survey area displayed an average total carbon content of 1.18%, an average total carbon density of 34.27 t/hm2, an average organic carbon content of 1.07%, and an average organic carbon density of 30.94 t/hm2. With annual average increases in the total carbon density and organic carbon density of 9.642 t/hm2 and 4.727 t/hm2, respectively, this year witnessed increases in the total carbon and organic carbon of -2,410.5 kg/(hm2·a) and 1,181.75 kg/(hm2·a), respectively. The respective reserves of total carbon and organic carbon were 1.963 5 million tons and 1.772 61 million tons. The total carbon reserves in topsoils in the whole study area were 14.474 81 million tons, including organic carbon reserves of 10.652 2 million tons. The total carbon reserves decreased by 552.41 thousand tons, while the organic carbon reserve increased by 270.82 thousand tons. Overall, the study area experienced a total carbon decrease of 354.13 thousand tons and an increase in the organic carbon reserves of 2.128 62 million tons. The total carbon showed significant positive correlations with the contents of organic carbon, CaO, MgO, N, and P, the organic carbon displayed significant positive correlations with the contents of total carbon, N, and P, and there was a significant positive correlation between pH and the CaO content. Fertilization led to an increase in the organic carbon and total carbon contents in farmland soils, with total carbon being significantly affected by the CaO content. In the carbonate areas, alkaline soil environments exhibited carbon sink characteristics. In the southern regions with acidified soil environments, the decomposition of carbonates in soils led to carbon loss and reduced calcium content. The results of this study provide important scientific evidence for research on peak carbon dioxide emissions and carbon neutrality of Luoyang City.

       

    /

    返回文章
    返回