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    近20年“三北”工程内蒙古阻击战区风沙活动特征与治理成效

    Wind-sand activity characteristics and control effectiveness in the Inner Mongolia sector of the Three-North Counter-Sand Campaign over the past 20 years

    • 摘要: 摘要:风蚀是干旱区土地退化与荒漠化的主导过程之一,对区域生态安全构成严重威胁。位于内蒙古“三北”阻击战的巴丹吉林—腾格里沙漠交错区地处中国西北风沙活动最频繁、生态环境最脆弱的地带,其风蚀演变规律与防治对策需要系统研究。文章基于2000-2024年多期遥感数据,结合土地利用动态度、土地利用转移矩阵与修正风蚀方程(RWEQ)模型,从土地利用格局变化、土壤风蚀模数演变及风蚀强度等级转换等方面展开定量分析,并进一步提出分区化治理措施。结果表明:(1)研究区以裸地为主,占比始终超过94%,草地与农田面积在时序上呈阶段性波动,但近年有一定恢复趋势;(2)土壤风蚀模数表现出阶段性波动特征,2000年为3905.96t/(km²·a),2024年升至4360.95t/(km²·a),峰值高达15532.87t/(km²·a);(3)空间格局上,强烈与极强烈风蚀区集中分布于两大沙漠边缘,2024年合计面积达11813.31km²,占比超过41%;(4)风蚀等级转换显示,2000-2024年高等级风蚀面积增加5660km²,但低等级风蚀转化比例逐渐上升,表明治理措施和植被恢复取得初步成效。综上,研究区风蚀过程呈现明显的阶段性波动,部分区域在治理措施下已得到缓解,但沙漠边缘地带仍是防控重点。文章提出的“工程防沙前沿区、综合固阻体系区、自然封育保育区”分区,为“三北工程”阻击战及区域差异化防沙治沙提供了科学支撑与实践指导。

       

      Abstract: Abstract:BackgroundWind erosion is a primary driver of land degradation and desertification in arid regions, posing a serious threat to regional ecological security. Situated within the Inner Mongolia sector of China’s “Three-North” Counter-Sand Campaign, the Badain Jaran–Tengger desert ecotone lies in one of the countrys most wind-active and ecologically fragile belts, where the dynamics of wind erosion and control strategies warrant systematic study.MethodsUsing multi-temporal remote-sensing datasets (2000–2024) in combination with land-use dynamic degree analysis, land-use transfer matrices, and the Revised Wind Erosion Equation (RWEQ) model, this study quantitatively assesses shifts in land-use patterns, trajectories of the soil wind-erosion modulus, and transitions among wind-erosion intensity classes, and further proposes a zoned control scheme.Results1) the study area is dominated by bare land, consistently exceeding 94% of the total area; grassland and cropland display stage-like fluctuations but a modest recovery in recent years; 2) the soil wind-erosion modulus exhibits pronounced phase fluctuations, rising from 3,905.96 t·km⁻²·a⁻¹ in 2000 to 4,360.95 t·km⁻²·a⁻¹ in 2024, with a peak of 15,532.87 t·km⁻²·a⁻¹; 3) spatially, strong and very strong erosion zones cluster along the margins of the two deserts, totaling 11,813.31 km² in 2024 (>41% of the region); (4) intensity-class transitions indicate a net increase of 5,660 km² in higher-grade erosion from 2000 to 2024, while the share shifting toward lower grades has grown in recent years, implying emerging benefits from control measures and vegetation recovery. Overall, wind-erosion processes exhibit marked stagewise fluctuations; some areas have been alleviated under interventions, yet desert margins remain priority targets.ConclusionThe proposed three-zone scheme—“engineering sand-control frontline, integrated fixation-and-retardation system, and conservation-oriented enclosure”—provides scientific support and practical guidance for the Three-North Project’s campaign and for differentiated sand-control practices in the region.

       

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