4.7 Article

Characteristics and predictive models of hillslope erosion in burned areas in Xichang, China, on March 30, 2020

Journal

CATENA
Volume 217, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.catena.2022.106509

Keywords

Wildfire; Hillslope erosion depth; Post -fire debris flow; Predictive model; Sediment Delivery Ratio

Funding

  1. National Natural Science Foundation of China
  2. State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, China
  3. Program of Science and Technology Department of Sichuan Province, China
  4. [41731285]
  5. [41907225]
  6. [SKLGP2018K011]
  7. [2021YJ0033]

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This study analyzed post-fire hillslope erosion using various methods, developed a predictive model, and evaluated the model performance. The results show that fire severity, soil properties, rainfall, and topography are the main factors affecting hillslope erosion, and the new predictive model has a good performance.
Wildfires often greatly aggravate hillslope erosion, which is a complex, highly dynamic and constantly changing water-soil interaction process. In this study, the remote sensing interpretation, field investigation, in-situ soil erosion pins experiments, and laboratory test were used to examine the controlling factors of post-fire hillslope erosion after the Xichang Fires occurred on March 30, 2020, in southwest Sichuan Province, China. We devel-oped an empirical model to predict predicting post-fire hillslope erosion, and evaluated the model performance at watershed scale combined with the Sediment Delivery Ratio model (SDR). The controlling factors of hillslope erosion (fire severity, soil properties, rainfall, and topography) were collected. The correlations between rainfall events-based hillslope erosion depth (HED) and the controlling factors were examined. The results show that the fire severity has the strongest correlation, followed by soil properties, rainfall, and topography. The new pre-dictive models were developed using multiple linear and non-linear (power law relationship) regression based on the normalized differenced Normalized Burn Ratio (ndNBR), soil erodibility (K), accumulated rainfall erosivity ( n-ary sumation R) and topographic factor (LS). Then, the methods were evaluated by comparing the predicted and observed values on the testing subset based on the statistical coefficients including R-squared, root mean squared error (RMSE) and discrepancy ratio (DR). The results suggest that the developed empirical model based on multiple non-linear (power law relationship) has a better performance (R-squared: 0.600, RMSE: 1.948), and the discrepancy ratio of 87.2% data range from 0.5 to 2. The model was used to estimate the spatial distribution of hillslope erosion depth across the entire study area, and the sediment yield at watershed scale (WSY) combined with the SDR model. The comparison between the observed sediment mobilized by debris flow and the predicted WSY shows that the model combined with the SDR showed an acceptable performance at watershed scale.

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