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宁夏引黄灌区土壤有机碳密度时空变化特征

董林林,于东升**,张海东,史学正   

  1. (中国科学院南京土壤研究所土壤与农业可持续发展国家重点实验室, 南京 210008)
  • 出版日期:2015-08-10 发布日期:2015-08-10

Temporal and spatial changes of soil organic carbon density in Ningxia Irrigation Zone from 1980 to 2009.

DONG Lin-lin, YU Dong-sheng**, ZHANG Hai-dong, SHI Xue-zheng   

  1. (State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China)
  • Online:2015-08-10 Published:2015-08-10

摘要: 利用1980年全国第二次土壤普查的102个土壤剖面(0~100 cm)和147个表层样(0~20 cm),以及2009年采集的39个土壤剖面和241个表层土样属性数据,分别计算灌区表层和剖面土壤有机碳密度,通过对比分析,研究了宁夏引黄灌区近30年来土壤有机碳储量的变化特征。结果表明:1980—2009年,宁夏引黄灌区表层(0~20 cm)土壤有机碳密度由16.57 Mg C·hm-2增至21.44 Mg C·hm-2,平均年增幅为0.98%(P<0.01);剖面(0~100 cm)土壤有机碳密度平均由55.70 Mg C·hm-2增至58.49 Mg C·hm-2,平均年增幅为0.17%(P>0.05);土壤类型是影响灌区土壤有机碳储量的主导性因素;灌区土壤有机碳密度与灌溉时间之间有较强的相关性(P<0.01),灌溉耕作时间越长,土壤有机碳密度越高;单位面积化肥施用量、单位面积作物产量及作物种植类型对灌区土壤有机碳变化产生了重要影响;气温和降水对土壤有机碳变化影响不明显。引黄灌溉耕作对提高灌区土壤有机碳储量和降低温室气体排放具有积极的作用。

关键词: 适生分布区, 气候变化, 翅果油树, Maxent

Abstract: In the Ningxia Irrigation Zone, 39 samples of soil profiles (0-100 cm) and 241 samples of surface layers (0-20 cm) were collected in 2009, and soil data attributing to 102 samples of profiles and 147 samples of surface layers were collected, which were obtained from the Second National Soil Survey of China in 1980. Then, soil organic carbon (SOC) densities in the surface layer and profile depth were calculated for the analysis of SOC stock change during the past 30 years. The results showed that SOC density of surface layer had increased significantly (P<0.01) from 16.55 Mg C·hm-2 in 1980 to 21.44 Mg C·hm-2 in 2009, with an annual increase of 0.98%. The SOC density in profile increased (P>0.05) from 55.70 Mg C·hm-2 to 58.49 Mg C·hm-2 with an annual increase of 0.17% during the past 30 years. Soil type was a major factor driving the change of SOC stock in the Ningxia Irrigation Zone. A strong relationship was found between SOC density and irrigation duration, indicating that irrigation had a prominent effect on SOC density change, the longer duration of irrigation, the higher density of SOC in the surface layer and profile. Fertilizer input, crop type and yield also affected the change of SOC density in the irrigated cropland. Non-significant relationship was found between SOC density and climate index such as air temperature and precipitation. Irrigation with Yellow River water plays a positive role in increasing SOC stock and decreasing greenhouse gas emission in Ningxia Irrigation Zone.

Key words: suitable distribution, Maxent, climate change., Elaeagnus mollis