黄土高原丘陵沟壑区坡耕地撂荒后自然恢复草地碳动态

发布时间:2021-06-29 09:33
  黄土高原大规模的退耕还林还草促进了生态恢复。但是长期来看,树种的生长消耗土壤水分,致使土壤表层形成了干化层,最终导致林地退化。自然植被演替表现出越来越强的生态适应性,加速自然植被的演替可以加速生态恢复。本研究以黄土高原自然恢复草地为研究对象,通过野外调查和实验室分析,选取典型样地对植被和土壤碳库变化动态进行了研究,提出了加速草地恢复和增加土壤碳汇的对策和措施。本研究为自然草种演替增加土壤碳汇、恢复生态环境提供了重要的科学依据。本研究取得的主要结论如下:(1)草地恢复加强了土壤碳库的积累,包括土壤有机碳库和无机碳库,但是这两个碳库在总碳库的占比相反。与农田相比,土壤有机碳储量(0-100 cm)在草地恢复的早期显著降低,土壤无机碳储量(0-100 cm)在农田撂荒后早期显著增加。土壤无机碳储量恢复较之有机碳储量恢复快。与农田相比,0-100cm土层土壤有机碳储量增量分别为-0.039(5年),0.037(13年),0.840(24年)和1.082 kg m-2(32年);0-100cm土层土壤无机碳储量增量分别为1.209(5年),6.000(13年),6.608(24年),and 4.... 

【文章来源】:西北农林科技大学陕西省 211工程院校 985工程院校 教育部直属院校

【文章页数】:103 页

【学位级别】:博士

【部分图文】:

黄土高原丘陵沟壑区坡耕地撂荒后自然恢复草地碳动态


979年以来全球主要温室气体(CO2,N2O,CH4)平均丰度变化(NOAAglobalairsamplingnetwork)http://www.esrl.noaa.gov/gmd/ccgg/aggi.html

化石燃料,水泥,来源,文献综述


第一章 文献综述 3图1-2 化石燃料和水泥使用,土地利用变化导致的CO2释放速率变化。来源: CDIAC; Le Quéré et al2014; Global Carbon Budget 2014Figure 1-2 The changes of CO2emissions induced by fossil fuels and cement, land-use change图1-3 主要国家和组织化石燃料使用造成的CO2释放量。来源:CDIAC; Le Quéré et al 2014; GlobalCarbon Budget 2014Figure 1-3 The changes of CO2emissions induced by fossil fuels for top four emitters. Source: CDIAC; LeQuéré et al 2014; Global Carbon Budget 2014

主要国家,CO2释放量,来源


2emissions induced by fossil fuels and cement, land-use change图1-3 主要国家和组织化石燃料使用造成的CO2释放量。来源:CDIAC; Le Quéré et al 2014; GlobalCarbon Budget 2014Figure 1-3 The changes of CO2emissions induced by fossil fuels for top four emitters. Source: CDIAC; LeQuéré et al 2014; Global Carbon Budget 2014

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