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陕西省农田土壤生态系统碳汇时空演变特征

Spatial-temporal Evolution Characteristics of Carbon Sink in Farmland Soil Ecosystem in Shaanxi Province

  • 摘要: 在2005—2020年陕西省农田土壤生态系统碳汇测算的基础上,采用标准差椭圆、空间自相关、冷热点分析等方法,对其碳汇时空演变特征进行研究,以期揭示土壤碳汇时空异质性,合理制定区域适宜的农田管理政策。结果表明:1)2005—2020年陕西农田土壤碳汇总量整体呈波动上升趋势,碳汇量从每年的58.83×10~4 t上升至76.51×10~4 t;碳汇类型以施用肥料碳汇为主。2)空间上呈现“中间高,南北低”的分布格局。高值区域主要分布在咸阳、渭南、西安和宝鸡,低值区域分布于榆林、安康和商洛。3)空间分布重心整体存在向北略东移动的趋势,分布范围呈先收缩后扩张的态势,西北地区对整体碳汇空间格局影响作用加强。土壤碳汇强度具有空间正相关性,冷热点空间分布集聚程度呈现波动稳定的特征。

     

    Abstract: Based on the estimation of carbon sink of farmland soil ecosystem in Shaanxi Province from 2005 to 2020,used the methods of standard deviation ellipse, spatial autocorrelation, cold and hot spot analysis to study the spatial-temporal evolution characteristics of its carbon sink, in order to reveal the spatiotemporal heterogeneity of soil carbon sink and reasonably formulate regional appropriate farmland management policies.The results showed that, 1) From 2005 to 2020,the total amount of soil carbon sink in Shaanxi farmland showed a fluctuating upward trend, from 58.83×10~4 t per one year to 76.51×10~4 t per one year.The type of carbon sink was mainly fertilizer carbon sink.2) The spatial distribution pattern was ‘high in the middle and low in the north and south’.High-value areas were mainly distributed in Xianyang, Weinan, Xi′an and Baoji, while low-value areas were distributed in Yulin, Ankang and Shangluo.3) The center of gravity of the spatial distribution had the trend of moving to the north and slightly to the east, and the distribution scope had the trend of contracting first and then expanding.The influence of the northwest region on the overall spatial pattern of carbon sinks had been strengthened.The intensity of soil carbon sink had a positive spatial correlation, and the spatial distribution and concentration of cold and hot spots showed a fluctuating and stable feature.

     

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