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Landscape Architecture Frontiers

ISSN 2096-336X

ISSN 2095-5413 (Online)

CN 10-1105/TU

邮发代号 80-985

Landscape Architecture Frontiers  2024, Vol. 12 Issue (3): 10-26   https://doi.org/10.15302/J-LAF-0-020017
  本期目录
Research on the Territorial Ecological Restoration of Counties for the Increase of Carbon Sinks—A Case Study of Wensu County, Xinjiang Uygur Autonomous Region, China
Qingwen ZHANG, Ying YANG, Yi YUAN, Jingyi HAN, Dihua LI()
College of Architecture and Landscape, Peking University, Beijing 100080, China
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Abstract

As global climate continues to change, it is pressing to integrate the carbon peaking and carbon neutrality goals into territorial spatial planning. While little existing ecological restoration research focuses on counties in western China, particularly arid areas of northwest China, this research took Wensu County of the Xinjiang Uygur Autonomous Region in China as the study case, evaluated the carbon sequestration capacity and carbon storage of the current carbon sinks, identified the spatial pattern of carbon sinks, and proposed the territorial ecological restoration approaches to increasing carbon sinks. The evaluation results show that the importance level of carbon sinks varies significantly across geographical environments of the county, where one primary carbon sink, two secondary carbon sinks, and potential carbon sinks with a total area of 2259.81 km2 were identified. This research extracted eight typical land use patterns based on current land use and proposed ecological restoration strategies accordingly. This research shows a way to integrate carbon peaking and carbon neutrality goals in territorial spatial planning, which is instrumental for carbon sink management in the arid areas of northwest China and provides a referable paradigm for regions with similar geographical conditions.

● Focuses on ecological restoration in a county in the arid areas of northwest China, aiming for carbon sink increase

● Evaluates the carbon sequestration and storage patterns of current carbon sinks in the study area and identifies the spatial pattern of carbon sink importance level

● Extracts typical land use patterns based on current land use and proposes ecological restoration strategies accordingly

Key wordsCarbon Sink Increase    Carbon Sequestration    Carbon Storage    County Region    Arid Areas of Northwest China    Ecological Restoration    Territorial Spatial Planning
收稿日期: 2023-01-17      出版日期: 2024-06-28
Corresponding Author(s): Dihua LI   
 引用本文:   
. [J]. Landscape Architecture Frontiers, 2024, 12(3): 10-26.
Qingwen ZHANG, Ying YANG, Yi YUAN, Jingyi HAN, Dihua LI. Research on the Territorial Ecological Restoration of Counties for the Increase of Carbon Sinks—A Case Study of Wensu County, Xinjiang Uygur Autonomous Region, China. Landsc. Archit. Front., 2024, 12(3): 10-26.
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https://academic.hep.com.cn/laf/CN/10.15302/J-LAF-0-020017
https://academic.hep.com.cn/laf/CN/Y2024/V12/I3/10
Fig.1  
DatasetData typeSpatial resolutionData source
Land useRaster1 kmResource and Environment Science and Data Center, Chinese Academy of Sciences
Net primary production (NPP)Raster500 mUnited States Geological Survey
Digital elevation model (DEM)Raster30 mGeospatial Data Cloud
Monthly mean temperatureRaster1 kmResource and Environment Science and Data Center, Chinese Academy of Sciences
Monthly total precipitationRaster1 kmResource and Environment Science and Data Center, Chinese Academy of Sciences
Spatial distribution of population densityRaster1 kmWorldPop
Spatial distribution of vegetation typesVector1∶1,000,000Resource and Environment Science and Data Center, Chinese Academy of Sciences
China's soil dataset from Harmonized World Soil Database (v 1.1)Raster1 kmNational Tibetan Plateau Data Center
Tab.1  
Fig.2  
Vegetation typeVegetation subtypeCarbon density(t/hm2)Area(×104 hm2)Carbon storage(×104 t)
Coniferous forestCool temperate and temperate montane coniferous forest52.31.0957.007
ScrubSubalpine deciduous broad-leaved scrub7.70.221.694
DesertTemperate shrub desert1.027.6727.670
Temperate steppe shrub desert1.00.800.800
Temperate subshrub and dwarf subshrub desert1.013.4913.490
Temperate succulent halophyte dwarf subshrub desert1.04.164.160
SteppeTemperate bunch grass typical steppe2.19.0519.005
Temperate grass and forb meadow steppe2.12.114.431
Temperate bunch short grass and dwarf subshrub desert steppe2.14.579.597
MeadowTemperate grass and forb halophyte meadow3.724.0789.059
Temperate grass, sedge, and forb marsh meadow3.90.070.273
Alpine Kobresia and forb meadow1.83.506.300
Alpine vegetationAlpine cushion-like vegetation3.30.652.145
Alpine talus vegetation3.318.2060.060
Cultivated vegetationTwo-year triple cropping or one-year double cropping dry farming and deciduous orchard5.711.4665.322
Non-vegetation area0.021.040.000
Total142.15361.013
Tab.2  
Fig.3  
CategoryDescription
Primary carbon sink· Continuous carbon sinks that are mostly rated as "very high" and "high" level of importance, critical to maintaining and increasing carbon sinks
· They are mostly covered by natural vegetation with little human intervention, featuring a healthy ecosystem and abundant natural endowments
· Ecological protection should be prioritized
Secondary carbon sink· Continuous carbon sinks that are rated as "high" level of importance
· They are mainly covered by cultivated vegetation
· It requires site-specific ecological protection and restoration approaches
Potential carbon sink· Areas between the primary and secondary carbon sinks, rated as "moderate, " "low, " and "very low" level of importance
· They are mainly covered by natural vegetation, surrounded by large areas of unused land such as Gobi desert and bare rock or gravel; the vegetation is in fair condition, easily to be disturbed and generate carbon emissions
· Key areas to increase carbon sinks with gradual ecological restoration while avoiding large amount of carbon emissions from disturbances
Tab.3  
Resistance factorInformation entropy (e)Difference coefficient (d)Weight (w)
Slope0.88980.110228.8111%
Elevation0.87580.124232.4634%
Land use0.96800.03208.3713%
Annual accumulated temperature0.91010.089923.4966%
Annual precipitation0.98810.01193.1203%
Population density0.98570.01433.7373%
Tab.4  
Resistance factorLevelValue
Slope (°)< 201
[20, 40)3
[40, 60)5
[60, 80)7
≥ 809
Elevation (m)< 2,0001
[2,000, 3,000)2
[3,000, 4,000)4
[4,000, 5,000)6
[5,000, 6,000)8
≥ 6,00010
Land useForest1
Grassland1
Farmland3
Water area5
Urban land, rural settlement, and other development land10
Unused land5
Annual accumulated temperature (℃)≥ 4,0001
[3,000, 4,000)3
[2,000, 3,000)5
[1,000, 2,000)7
< 1,0009
Annual precipitation (mm)≥ 6001
[450, 600)3
[300, 450)5
[150, 300)7
< 1509
Population density (people per square kilometer)< 1, 0001
[1000, 2000)3
[2000, 3000)5
[3000, 4000)7
≥ 4,0009
Tab.5  
Fig.4  
Fig.5  
Land use typeLand use subtypeManagement approaches
ForestForest land, shrub land, open forest land, other forest landAfforestation and reforestation, converting farmland to forest, natural forest protection, forest tending, naturalization of man-made forests, mixed forest plantation, agroforestry
GrasslandHigh coverage grassland, medium coverage grassland, low coverage grasslandNatural grassland enclosure, converting farmland to grassland, degraded grassland restoration, perennial mixed grassland interplanting, grazing intensity control, rotational grazing, deferred grazing
FarmlandPaddy land, dry landStraw mulching, applying organic fertilizers, conservation tillage, farmland rotation, irrigation management, composite system intercropping, recycling wasted farmland resources
Water areaRiver and canal, lake, reservoir, glacier and perennial snowfield, floodplainWetland conservation, degraded floodplain restoration, wetland management, garbage disposal, artificial wetland construction
Unused landSandy land, Gobi desert, saline-alkali land, bare soil, bare rock or gravelSoil remediation and maintenance, planting saline-tolerant and sand-fixing species, introducing new biotechnology to cultivate species (trees, grasses, or microorganisms) that can adapt to local conditions and efficiently sequestrate carbon
Tab.6  
Fig.6  
Fig.7  
Fig.8  
Fig.9  
Fig.10  
Fig.11  
Fig.12  
Land use subtypeArea (km2)PercentageTotal area (km2)
Dry land2.880.27%1,083.87
Forest land41.293.81%
Shrub land0.120.01%
Open forest land36.543.37%
High coverage grassland526.7948.60%
Medium coverage grassland124.4511.48%
Low coverage grassland344.2631.76%
River and canal5.700.53%
Floodplain1.840.17%
Tab.7  
Land use subtypeArea (km2)PercentageTotal area (km2)
Paddy land4.650.24%1,899.69
Dry land1,645.6586.63%
Forest land0.120.01%
Other forest land51.652.72%
High coverage grassland15.160.80%
Medium coverage grassland12.210.64%
Low coverage grassland78.794.15%
River and canal8.180.43%
Reservoir0.570.03%
Floodplain13.550.71%
Urban land2.210.12%
Rural settlement65.663.46%
Gobi desert0.310.01%
Bare soil0.980.05%
Tab.8  
Land use subtypeArea (km2)PercentageTotal area (km2)
Dry land16.130.71%2,259.81
High coverage grassland5.110.23%
Medium coverage grassland146.406.48%
Low coverage grassland1,158.7351.28%
Gobi desert330.8414.64%
Bare soil41.881.85%
Bare rock or gravel560.7224.81%
Tab.9  
Fig.13  
CategorySpatial pattern of land useCharacteristicEcological restoration strategyApproach
Primary carbon sinkForest–grasslandContinuous grassland scattered with forest patchesHigh-carbon reinforcementConserving existing carbon pools, restoring soil fertility, and increasing grassland carbon sink and storage by growing mixed forest on abandoned grasslands, forestation and reforestation, grazing intensity control, and natural grassland enclosure
Secondary carbon sinkGobi–farmland–grasslandContinuous Gobi desert with floodplain, grassland, and farmland along the bordersCarbon conservation restorationIncreasing the above-ground biomass, restoring soil fertility, conserving existing soil carbon pools, and enhancing grassland carbon sink via boundary restoration, floodplain ecological conservation, degraded grassland reseeding and maintenance, and converting farmland to grassland
Farmland–forest land–rural settlementContinuous farmland with scattered rural settlements and plantationsLow-carbon developmentRecycling the agricultural, forest, and residential resources, reducing resource consumption, and enhancing farmland carbon sequestration and storage (soil and vegetation) via conservation tillage, agroforestry, and agricultural waste recycling
Potential carbon sinkBare rock or gravel–grasslandBare rock or gravel areas with belts of low-coverage grasslandCarbon conservation expansionMaintaining natural succession, restoring soil fertility, and thus enhancing grassland carbon sink by soil mediation and maintenance of saline-alkali land, planting saline-tolerant and sand-fixing vegetation, and building shelterbelts along the boundaries
Grassland–bare soilContinuous low-coverage grassland interspersed with few bare soil areasReplanting for carbon sequestrationIncreasing grassland carbon sink (soil and vegetation), the above-ground biomass, and then carbon sink and storage of the region via bare soil land management, grazing management, and ecological replanting
Floopplain–saline-alkali landFloodplain near river and canals, bordered by saline-alkali land with sparse vegetationRestoring for carbon sequestrationImproving soil fertility and maintaining soil carbon pool by soil mediation and maintenance of the saline-alkali land, planting saline-tolerant species, and introducing new planting technologies
Forest–farmland–water areaShrub land–dry land–river and canal patches, with roads traversing throughMaintaining high carbon storageMaintaining soil carbon pool and boosting vegetation carbon sink by conservation tillage, converting farmland to forest, naturalization of man-made forests, and mixed forest plantation
Grassland–highwayNarrow low-coverage grassland belts traversing bare rock or gravel areas, with highways in the centerCarbon sequestration monitoringMaintaining grassland carbon pool (soil and vegetation) by natural grassland enclosure, rotational grazing, grazing intensity control, and shelterbelt construction; maintaining area carbon sink by planting along the highway
Tab.10  
Fig.14  
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