Morphological characteristics of permanent gullies and their relationship with topography in two typical agro-geomorphic regions of Northeast China

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Zhuoxin Chen, Qingchen Song, Mingming Guo, Pengchong Zhou, Lixin Wang, Qiang Chen, Xingyi Zhang
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Abstract

Gully erosion poses significant challenges to land degradation and food security. The Mollisols region of Northeast China (MNC) is the main grain-producing region in China. The low mountainous and hilly region (MFI) and the rolling hilly region (RFI), as the prominent topographic units in MNC, have suffered significantly from severe gully erosion. However, the actual situation and influencing factors of gully erosion in both regions are still unclear. Thus, we selected two field investigation regions of 103.4 km2 in MFI and 123.9 km2 in RFI to obtain a detailed inventory of gullies. Results showed that the gully number density in MFI was 25.7 No. km−2, 8.3 times greater than in RFI. Conversely, the gully average gully length (511.7 m), width (7.8 m) and depth (2.8 m) in RFI were 156.8%, 112.6% and 37.4% greater than those in MFI, respectively. The three types of gullies, developed in different land uses (GF, farmland; GW, woodland; GR, unpaved road), had significantly varying morphologies. In RFI, GF was the longest, and GW was the widest and deepest. Conversely, in MFI, GR was the longest but exhibited the least width and depth. Notably, farmland posed the highest risk of gully erosion in both MFI and RFI, with 74.4% and 89.6% of the gullies developed there, respectively. Topography was the critical factor influencing the differences in gully erosion between the two regions. To effectively control gully erosion, topographic conditions most susceptible to gully erosion should be prioritized for attention, e.g., slopes of 8–10° and 2–4° were the slope intervals most likely to contribute to gully development in MFI and RFI, respectively. We provide the potential for large-scale prediction of gully erosion. Corresponding prediction models based on gully area were provided and the effectiveness of the predictions was improved by separating different land uses. The study's findings could serve as a valuable foundation for gully erosion control and prediction for MNC.

东北两个典型农业地貌区永久沟壑形态特征及其与地形的关系
沟壑侵蚀对土地退化和粮食安全构成重大挑战。东北旱区是中国主要的粮食产区。低山丘陵区(MFI)和起伏丘陵区(RFI)作为跨国公司的主要地形单元,遭受了严重的沟壑侵蚀。但两区沟蚀的实际情况及影响因素尚不清楚。因此,我们选择了MFI 103.4 km2和RFI 123.9 km2的两个实地调查区域,以获得详细的沟渠清单。结果表明:MFI沟壑数密度为25.7条;km−2,是RFI的8.3倍。相反,RFI的平均沟长(511.7 m)、沟宽(7.8 m)和沟深(2.8 m)分别比MFI高156.8%、112.6%和37.4%。三种类型的沟渠,在不同的土地利用(GF,农田;GW,林地;GR(未铺砌道路)的形态差异显著。在RFI中,GF最长,GW最宽最深。相反,在MFI中,GR最长,但宽度和深度最小。值得注意的是,农田沟槽侵蚀风险最高,分别占74.4%和89.6%。地形是影响两区沟蚀差异的关键因素。为了有效控制沟壑侵蚀,应优先关注最易受沟壑侵蚀的地形条件,例如,在MFI和RFI中,8-10°和2-4°的坡度区间分别是最有可能促进沟壑发育的坡度区间。我们提供了大规模预测沟蚀的潜力。建立了基于沟壑区面积的预测模型,并通过对不同土地利用方式的分离,提高了预测的有效性。研究结果可为跨国公司的沟沟侵蚀控制和预测提供有价值的基础。
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来源期刊
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms 地学-地球科学综合
CiteScore
6.40
自引率
12.10%
发文量
215
审稿时长
4 months
期刊介绍: Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with: the interactions between surface processes and landforms and landscapes; that lead to physical, chemical and biological changes; and which in turn create; current landscapes and the geological record of past landscapes. Its focus is core to both physical geographical and geological communities, and also the wider geosciences
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