globalchange  > 气候变化与战略
CSCD记录号: CSCD:5522099
论文题名:
黄土高原羊圈沟小流域土地利用时空变化的土壤有机碳效应
其他题名: Effects of spatio-temporal changes of land-use on soil organic carbon in Yangjuangou watershed in Loess Plateau, China
作者: 文雯1; 周宝同2; 汪亚峰1; 梁地1
刊名: 生态学报
ISSN: 1000-0933
出版年: 2015
卷: 35, 期:18, 页码:161-169
语种: 中文
中文关键词: 土地利用变化 ; 土壤有机碳 ; 羊圈沟小流域 ; 黄土丘陵地区
英文关键词: land use change ; soil organic carbon ; yangjuangou watershed ; loess plateau
WOS学科分类: BIOLOGY
WOS研究方向: Life Sciences & Biomedicine - Other Topics
中文摘要: 土地利用变化是影响土壤有机碳储量和分布变化的重要驱动因素,为进一步探讨土地利用变化对土壤有机碳的影响,根据土壤样点数据、土地利用类型图,分析了黄土丘陵沟壑区羊圈沟小流域2006-2011年土地利用变化及其对表层土壤有机碳密度和储量的影响,主要结论如下:(1)小流域土地利用发生较大变化,主要集中在乔木林地和灌木林地面积的增加,分别为39.697、46.404hm~2;以及草地面积的减少,为64.030hm~2;(2)土地利用方式的变化会导致土壤有机碳密度及储量的变化,其中转变用地类型的土壤有机碳储量增加587.25kg,以荒草地转出类型增加的土壤表层有机碳储量最多,为441.64kg;灌木林地转出类型减少的土壤表层有机碳储量最多,为-21.01kg。草地-灌木林地、草地-乔木林地、坡耕地-草地、坡耕地-灌木林地、坡耕地-乔木林地、坡耕地-坝地、梯田-草地、梯田-灌木林地、梯田-乔木林地、梯田-坝地、坝地-草地、坝地-灌木林地、坝地-乔木林地等转换用地类型的表层土壤碳密度增加值高于保持用地类型碳密度的增加值,说明这些地类的转换有利于表层土壤有机碳储量的增加,即有利于表层土壤碳汇的形成;而其他地类转换造成了表层土壤的碳排放,应该引起足够的重视;(3)土壤固碳应着眼于长期效应,频繁的土地利用类型转化可能会降低土壤碳截流效果,黄土丘陵区植被重建的长期利用和保持更有利于土壤有机碳的积累。
英文摘要: Land use change is an important driving factor for changes of storage and spatial distribution of soil organic carbon (SOC). In order to study effects of land use change on SOC, we analyzed the spatio-temporal changes of land use and their effects on SOC content, density and storage of topsoil based on soil sampling data and land-use map from 2006 to 2011 in Yangjuangou watershed. The main conclusions include that, (1) Land use types in this watershed changed significantly from 2006 to 2011. The area of grass land, which mainly transformed into shrub land and arboreal land, decreased the most with 64.030 hm~2, following by sloping farmland mainly transformed into terrace; the area of shrub land and arboreal land increased rapidly by 39.697 hm~2, and 46.404 hm~2respectively, which were converted from the grass land, terrace, sloping farmland, dam land and construction land; the area of terrace was so small that the transformation was not obvious. (2) Land use change caused change of density and storage of SOC. The increase of carbon storage due to land type changes was 587.25 kg, among which the contribution from changed land types converted from grass land was 441.64 kg. Within all the land use transformations,' grass land to shrub land ',' grass land to arboreal land ', sloping farmland to grass land', sloping farmland to shrub land', sloping farmland to arbor land', sloping farmland to terrace', sloping farmland to terrace , terrace to grass land', terrace to shrub land', terrace to arboreal land , terrace to dam land', dam land to grass land ,' dam land to shrub land',and dam land to arboreal land' showed higher SOC densities than those of the original land use types. It indicated that these land use transformations were conducive to increase of surface SOC and reduction of carbon emissions, which were beneficial to formation of surface soil carbon sink. However, other land use transformations, which caused increase of surface soil organic carbon emissions, should be paid more attention to. (3) The content, density and storage of SOC didn't increase so much in Yangjuangou watershed from 2006 to 2011. Nevertheless, soil carbon sequestration should focus on the long-term effects, and frequent transformations of land use types may reduce the intercepting effect of soil carbon. The long-term utilization and maintain of vegetation reconstruction are much more conducive to accumulation of SOC in the Loess hilly-gully regions. Different transformations of land use types led to different regional changes of SOC storage. Those land use types which converted into shrub land and arboreal land contained the most SOC storage. Therefore, it is of extremely importance to protect forests to mitigate global warming, and the attention should be paid to afforestation and plantation tending management. Only seeking out a suitable mode of land resources management, which is beneficial to increase of sequestration of atmospheric CO_2 through soil and could reverse land degradation process, can it be the best choice for mitigating rising levels of CO_2.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/149845
Appears in Collections:气候变化与战略

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作者单位: 1.中国科学院生态环境研究中心, 城市与区域生态国家重点实验室, 北京 100085, 中国
2.西南大学地理科学学院, 重庆 400715, 中国

Recommended Citation:
文雯,周宝同,汪亚峰,等. 黄土高原羊圈沟小流域土地利用时空变化的土壤有机碳效应[J]. 生态学报,2015-01-01,35(18):161-169
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