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松嫩黑土区农田道路切沟空间分布特征及其影响因素

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[目的]侵蚀沟治理是黑土地保护工程的重点,但目前区域尺度道路切沟的分布格局尚未明确,严重阻碍侵蚀沟治理进程。为厘清区域尺度道路切沟分布特征及影响因素,[方法]以松嫩黑土区为例,系统布设886 个小流域单元,基于Google Earth亚米级遥感影像,综合运用反距离权重法、热点分析及随机森林模型特征选择,探究道路切沟空间特征及影响因素。[结果]结果显示:(1)松嫩黑土区 14。45%的抽样单元存在道路切沟,道路切沟平均长度 232。27 m,平均长度密度 0。11 km·km-2,平均沟数密度0。46 条·km-2。(2)道路切沟长度密度和沟数密度较大的地区分布于东北部的漫川漫岗地区(齐齐哈尔、绥化、黑河三市交界处和哈尔滨西北部)、东南部的低山丘陵地区(长春东北部)及西北部的山地丘陵地区(呼伦贝尔东南部与齐齐哈尔交界处)。(3)坡度、降水和海拔对道路切沟密度的贡献度表现为坡度>降水>海拔。4°~6°坡段、270~300 m海拔段,以及>600 mm降雨等级上,道路切沟分布最为密集。[结论]结果表明:除中部和西南地区外,均存在道路切沟且沿松嫩黑土区边界呈带状分布;坡度、降水和海拔是影响松嫩黑土区道路切沟形成和发育的主要因子,坡度为最主要因子;亚米级遥感影像目视解译结合系统抽样的方法在区域尺度道路切沟研究上具有可靠性和适用性,可为黑土区道路切沟治理和黑土资源保护工作提供理论支撑。
Spatial distribution characteristics and influencing factors of unpaved road gullies in the mollisol region of songnen
[Objective]Erosion gully management is a crucial aspect in the conservation of Mollisols,but the distribution pattern of unpaved road gullies at the regional scale has not yet been clarified,which seriously impedes the process of erosion gully man-agement.In order to clarify the distribution characteristics and influencing factors of unpaved road gullies at the regional scale,[Methods]taking the Songnen Mollisol region as an example,this paper systematically establishes 886 small watershed units and comprehensively uses the inverse distance weighted interpolation,hotspot analysis and random forest model feature selection to explore the spatial characteristics and influencing factors of unpaved road gullies based on high-resolution remote sensing images from Google Earth.[Results]The result show that:(1)14.45%of the sampled units in the Songnen Mollisol region have un-paved road gullies,with an average gully length of 232.27 m,average length density of 0.11 km·km-2,and average number density of 0.46 gullies·km-2.(2)Regions with high unpaved road gully length density and number density are distributed in the northeastern Manchurian plain region(at the junction of Qiqihar,Suihua,and Heihe,and the northwestern part of Harbin),the southeastern low mountainous region(northeast of Changchun),and the northwestern mountainous region(southeast of Hulunbuir and the junction of Qiqihar).(3)The contribution of slope gradient,precipitation and elevation to the unpaved road gully density showed slope gradient>precipitation>elevation.Unpaved road gullies are most densely distributed in the 4°~6° slope gradient range,the 270~300 m elevation range,and in areas with precipitation levels exceeding 600 mm.[Conclusion]The result show that:Except for the central and southwestern regions,there are unpaved road gullies and they are distributed in bands along the boundary of the Songnen Mollisol region;Slope gradient,precipitation,and elevation are the main factors influ-encing the formation and development of unpaved road gullies in the Songnen Mollisol region,with slope gradient being the most significant factor;The method of visual interpretation of sub-meter remote sensing images combined with systematic sampling is reliable and applicable to the study of unpaved road gullies at the regional scale,providing theoretical support for the management of unpaved road gullies and the protection of black soil resources in the region.

mollisol region of the Northeastsub-meter remote sensing imagegully erosionunpaved road gulliesinfluencing factorsprecipitation

刘兆题、王春梅、李芹芳、申华珍、张春妹、王强、龙永清、杨勤科

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长安大学 土地工程学院,陕西 西安 710054

西北大学 城市与环境学院 陕西省地表系统与环境承载力重点实验室,陕西 西安 710127

旱区生态水文与灾害防治国家林业和草原局重点实验室,陕西 西安 710048

东北黑土区 亚米级遥感影像 切沟侵蚀 道路切沟 影响因素 降水

2024

水利水电技术(中英文)
水利部发展研究中心

水利水电技术(中英文)

CSTPCD北大核心
影响因子:0.456
ISSN:1000-0860
年,卷(期):2024.55(10)