黄河流域生态功能区植被碳汇估算及其气候影响要素

Abstract

PDF HTML阅读 XML下载 导出引用 引用提醒 黄河流域生态功能区植被碳汇估算及其气候影响要素 DOI: 10.5846/stxb202203110591 作者: 作者单位: 作者简介: 通讯作者: 中图分类号: 基金项目: 水沙科学与水利水电工程国家重点实验室(清华大学)2021年对外开放基金(sklhse-2021-A-06);辽宁省兴辽英才项目资助;国家自然科学基金项目(52079060) Estimation of vegetation carbon sink in the Yellow River Basin ecological function area and analysis of its main meteorological elements Author: Affiliation: Fund Project: 摘要 | 图/表 | 访问统计 | 参考文献 | 相似文献 | 引证文献 | 资源附件 | 文章评论 摘要:基于改进的CASA模型和土壤呼吸模型,综合遥感数据、气象数据、植被数据等多源数据类型,以黄河流域为研究对象,估算生态功能区植被碳源/汇,探讨其时空变化及主要气候影响要素。结果显示:(1)黄河流域植被净初级生产力(NPP)在2000-2020年整体呈波动上升趋势,多年平均NPP值为317.18 gC m-2 a-1;林地＞耕地＞沼泽＞草地,水体、戈壁、风蚀劣地和裸沙地的NPP总体处于较低值。空间尺度上,黄河流域NPP呈现出南高北低的分布特点,高值区集中在黄土高原农业与草原生态区与汾渭盆地农业生态区交界处,空间差异显著。(2)土壤微生物呼吸量极大值出现2018年,为15.82 gC m-2 a-1,最小值出现在2004年为14.34 gC m-2 a-1;空间上呈现从东南往西北、从东往西依次递减的空间分布格局。(3)黄河流域总体呈碳汇属性(碳汇区域超过60%),年均固碳量约为111.02 MgC/a,年均排碳量为-9.96 MgC/a,年均净碳汇总量约为111.41 MgC/a。(4)黄河流域植被碳汇的形成与降水和太阳辐射的相关性最大,气温的影响面积仅占12.44%;当气温为30℃,降水150 mm,太阳辐射550 MJ/m2时,植被固碳能力效果最强。研究结果为区域全面准确地评估陆地生态系统碳源/汇,实现黄河流域高质量发展,达到碳中和目标提供参考依据。 Abstract:Based on the improved CASA (Carnegie-Ames-Stanford Approach) model and soil respiration model, this paper integrates multi-source data, such as remote sensing data, meteorological data and vegetation data, to estimate vegetation carbon sources/sinks in ecological function areas, and explore their spatio-temporal variations and main climate influencing elements in the Yellow River Basin. The results show that (1) the overall Net Primary Productivity (NPP) of vegetation in the Yellow River Basin presented a fluctuating upward trend from 2000 to 2020, with a multi-year average NPP value of 317.18 gC m-2 a-1. The NPP of various vegetation types showed that: forest land>cropland>swamp>grassland, and water bodies, Gobi, wind eroded poor land and bare sand land were at lower values overall. On the spatial scale, the NPP in the Yellow River Basin shows the distribution characteristics of high in the south and low in the north, and the high value areas are concentrated at the junction of the Loess Plateau agricultural and grassland ecological zone and the Fenwei Basin agroecological zone, with significant spatial differences. (2) The maximum value of soil microbial respiration appeared in 2018 at 15.82 gC m-2 a-1, and the minimum value appeared in 2004 at 14.34 gC m-2 a-1; spatially it showed a spatial distribution pattern decreasing from southeast to northwest and from east to west. (3) The Yellow River Basin has a carbon sink attribute in general (the carbon sink area exceeds 60%) The average annual carbon sequestration is about 111.02 MgC/a, the average annual carbon emission is -9.96 MgC/a, and the total annual net carbon sink is about 111.41 MgC/a. (4) The formation of vegetation carbon sink in the Yellow River Basin is mostly correlated with precipitation and solar radiation, and the influence area of air temperature only accounts for 12.44%; the effect of vegetation carbon sequestration capacity is the strongest when the temperature is 30℃, precipitation is 150 mm, and solar radiation is 550 MJ/m2. The results of the study provide a reference basis for a comprehensive and accurate regional assessment of carbon sources/sinks in terrestrial ecosystems to achieve high-quality development in the Yellow River Basin and meet the carbon neutrality target. 参考文献 相似文献 引证文献