Variation of soil properties induced by biochar amendments affects soil detachment capacity (D-c). However, the long-term effects of biochar on D-c have remained unexplored. This study assessed the variation of D-c with the rates and elapsed time since apple branch-derived biochar application, and quantified the relationship of D-c with hydrodynamic parameters and soil physicochemical properties in a three-year field experiment. Undisturbed soil samples to 20 cm depth were collected by using steel rings from field plots treated with biochar at 0, 24, 60, 96, 132, and 168 t ha(-1) after biochar application for 1, 2 and 3 years. The D-c of these samples was evaluated through a flume experiment, with scouring soil samples under three flow discharge rates (0.00025, 0.00045, and 0.00065 m(3) s(-1)) and five slope gradients (5.24, 8.75, 17.63, 26.79, and 40.40 %). Results revealed that, compared with no biochar treatment, the application of 24 similar to 96 t ha(-1) biochar after 1-2 years generally resulted in a reduction of D-c ranging from 6 %similar to 80 %, with a mean of 36 %. Conversely, 132 and 168 t ha(-1) biochar application increased D-c by 59 % and 45 %. All biochar treatments after 3 years resulted in a 48 % reduction in D-c relative to bare soil. The D-c generally decreased with an increasing of rates and elapsed time since biochar application. The mean weight diameter of soil aggregates (MWD) and cohesion (COH) were the key indices influencing D-c in the first two years, while total organic carbon (TOC) started to significantly affect D-c in the last year. Shear stress (tau) emerged as the optimal hydrodynamic parameter for simulating D-c. Power function equations well estimated D-c using tau, MWD, COH, and TOC under biochar application. These results demonstrate that applying biochar with sufficient elapsed time since application and low rates, rather than minimal elapsed time since application and high rates leads to a greater enhancement of soil erosion resistance for loess soils, with potential to control rill erosion for degraded or degrading sloping farmland at risk of erosion on the Loess Plateau. (c) 2025 International Research and Training Center on Erosion and Sedimentation, China Water and Power Press, and China Institute of Water Resources and Hydropower Research. Publishing services by Elsevier B.V. on behalf of KeAi Communications Co. Ltd. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).