A comparative study of long-term historical soil erosion in the four major Mollisols regions of the world

The Mollisols are among the world's most fertile soils but are increasingly threatened by erosion due to intensive cultivation and climate change. Despite their importance for global food production, the long-term dynamics of soil erosion in the four major Mollisols regions of the world as well as their comparisons and the control factors remain poorly understood. The Revised Universal Soil Loss Equation (RUSLE) was applied to estimate historical soil erosion from the 1900s to the 2020s across the four major global Mollisols regions, including the Mississippi Plain (MSP), the Northeast China Plain (NEC), the Pampas Plain (PP), and the Ukrainian Plain (UP). Scenario analysis, machine learning, and driver separation approaches were combined to quantify the contributions of driving forces to soil erosion during the past over 100 years. The results indicate that soil erosion has intensified across all regions during the past century. The NEC experienced the largest erosion intensity and increase, with mean erosion rates rising from 5 to 18.6 t·ha −1 ·yr −1 and a mean decadal increase of 0.95 t·ha −1 ·yr −1 , followed by the MSP (0.12 t·ha −1 ·yr −1 per decade), UP (0.11 t·ha −1 ·yr −1 per decade), and PP (0.10 t·ha −1 ·yr −1 per decade). Spatially, erosion expansion was widespread for all the four regions, particularly in mountainous and hilly landscapes, and LS-factor explained 35–55% of erosion variability. Scenario analysis indicated that land use change controlled long-term erosion trends in the NEC, climate-driven changes reproduced most of the observed increases in the UP, while both greatly affected erosion dynamics in the PP. In the MSP, erosion trajectories transitioned from land-use dominance in the early 20th century to increasing climate influence after the 1970s. These findings emphasize the urgent need for region-specific strategies to mitigate erosion risks in the four major Mollisols regions, especially for NEC.

Authors

Institutions

Publication Details

Journal
Ecological Indicators
Published
2026-09-16
DOI
https://doi.org/10.1016/j.ecolind.2026.115513
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
0.00

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
article

A comparative study of long-term historical soil erosion in the four major Mollisols regions of the world

Haiyan Fang, G.L. Tan
Ecological Indicators
Geology and Paleoclimatology Research
article

A comparative study of long-term historical soil erosion in the four major Mollisols regions of the world

Haiyan Fang, G.L. Tan
article en

Abstract

The Mollisols are among the world's most fertile soils but are increasingly threatened by erosion due to intensive cultivation and climate change. Despite their importance for global food production, the long-term dynamics of soil erosion in the four major Mollisols regions of the world as well as their comparisons and the control factors remain poorly understood. The Revised Universal Soil Loss Equation (RUSLE) was applied to estimate historical soil erosion from the 1900s to the 2020s across the four major global Mollisols regions, including the Mississippi Plain (MSP), the Northeast China Plain (NEC), the Pampas Plain (PP), and the Ukrainian Plain (UP). Scenario analysis, machine learning, and driver separation approaches were combined to quantify the contributions of driving forces to soil erosion during the past over 100 years. The results indicate that soil erosion has intensified across all regions during the past century. The NEC experienced the largest erosion intensity and increase, with mean erosion rates rising from 5 to 18.6 t·ha −1 ·yr −1 and a mean decadal increase of 0.95 t·ha −1 ·yr −1 , followed by the MSP (0.12 t·ha −1 ·yr −1 per decade), UP (0.11 t·ha −1 ·yr −1 per decade), and PP (0.10 t·ha −1 ·yr −1 per decade). Spatially, erosion expansion was widespread for all the four regions, particularly in mountainous and hilly landscapes, and LS-factor explained 35–55% of erosion variability. Scenario analysis indicated that land use change controlled long-term erosion trends in the NEC, climate-driven changes reproduced most of the observed increases in the UP, while both greatly affected erosion dynamics in the PP. In the MSP, erosion trajectories transitioned from land-use dominance in the early 20th century to increasing climate influence after the 1970s. These findings emphasize the urgent need for region-specific strategies to mitigate erosion risks in the four major Mollisols regions, especially for NEC.

Ecological IndicatorsVol. 191
Chinese Academy of Sciences (CN), Institute of Geographic Sciences and Natural Resources Research (CN), University of Chinese Academy of Sciences (CN)
National Natural Science Foundation of China
Life in Land
Openalex Percentile: Top 15%
Geology and Paleoclimatology Research
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.