Century-long spatiotemporal variation in cropland soil erosion and the roles of anthropogenic factors in the Tuojiang River Basin, China

IF 5.4 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Qi Wang , Yuchen Zhong , Wuhaomiao Yu , Zhaonan Tian , Xuesong Gao
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引用次数: 0

Abstract

Evaluating the long-term soil erosion dynamics and their responses to anthropogenic forcing at the regional level is crucial for assessing the impacts of soil conservation efforts and informing future policy development. The soil erosion issue is particularly severe in southwestern China due to its large hilly areas and extensive human activities. However, due to the lack of long-term records, there has been insufficient evaluation of the historical variations in cropland erosion across the spatial scales of decades and centuries, which hinders a comprehensive understanding of the main drivers and their effects. By using the Revised Universal Soil Loss Equation model in combination with remote sensing-based multisource data, the spatial and temporal evolution of cropland soil erosion in the Tuojiang River Basin (TRB) in China from 1911 to 2017 is assessed in this study. We also employ geographically and temporally weighted regression (GTWR) to assess the spatial and temporal heterogeneity of the anthropogenic factors impacting cropland soil erosion in the TRB from 1911 to 2017. The study results indicate that (1) in the past century, an average of 77.70% of the TRB has exhibited a slight soil erosion level, with the upper stream experiencing a higher rate. (2) The amount of soil erosion increased slightly from 1911 to 1960, dramatically increased by 70.07% from 1960 to 1980, and then decreased by 34.75% from 1980 to 2017. Cropland soil erosion mainly occurred in the upper stream, but it has been expanding to the downstream region since 2000. The high rate of cropland cultivation in the densely populated upper reaches is the main cause of accelerated erosion. (3) The increase in cropland soil erosion has primarily been driven by population growth and cropland expansion with contrary effects, reflecting a complex interplay of diverse natural and anthropogenic mechanisms. Spatiotemporal differentiations in the influences of both factors became evident with the economic reform and implementation of ecological conservation policies that have been occurring since 1980. These results can provide valuable insights for decision-makers for better understanding the long-term evolution of cropland soil erosion and the implementation of targeted soil conservation measures.

Abstract Image

沱江流域农田土壤侵蚀百年时空变化及人为因素的影响
在区域层面上评估土壤侵蚀的长期动态及其对人为强迫的响应对于评估土壤保持工作的影响和为未来的政策制定提供信息至关重要。中国西南地区由于山地多、人类活动频繁,水土流失问题尤为严重。然而,由于缺乏长期记录,对农田侵蚀在几十年和几个世纪的空间尺度上的历史变化评价不足,这阻碍了对主要驱动因素及其影响的全面认识。利用修正的通用水土流失方程模型,结合遥感多源数据,对1911 - 2017年中国沱江流域农田土壤侵蚀的时空演变进行了评价。利用地理和时间加权回归(GTWR)分析了1911 - 2017年青藏高原耕地土壤侵蚀人为因子的时空异质性。研究结果表明:(1)近百年来,平均77.70%的TRB呈现轻微的土壤侵蚀程度,上游土壤侵蚀程度较高;②1911 - 1960年土壤流失量略有增加,1960 - 1980年急剧增加70.07%,1980 - 2017年减少34.75%;耕地土壤侵蚀主要发生在上游,但自2000年以来已向下游扩展。在人口密集的上游地区,高耕地率是加速侵蚀的主要原因。(3)耕地土壤侵蚀的增加主要是由人口增长和耕地扩张驱动的,二者互为反作用,反映了多种自然和人为机制的复杂相互作用。随着1980年以来的经济改革和生态保护政策的实施,这两个因素影响的时空分异变得明显。这些结果可为决策者更好地了解农田土壤侵蚀的长期演变和实施有针对性的土壤保持措施提供有价值的见解。
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来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
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