peer reviewed ; Besides its carbon sequestration potential, biochar is being promoted as an amendment to improve soil quality. Burying biochar in soils is known to effect soil physical quality in the short-term (<5 years), although the intensity of these effects depends on soil texture. However, the long-term effects of biochar remain largely unknown yet are important to quantify given biochar’s persistency in soils. The objective of this study was therefore to assess the long-term effect of biochar on soil physical properties as a function of biochar concentration for soils with differing texture. For this purpose, soil physical properties were measured in the topsoil of three fields (silt loam, loam and sandy loam textures) in Wallonia (southern Belgium) presenting former kiln sites containing charcoal more than 150 years old. Particle density and bulk density slightly decreased as a function of charcoal-C content but the presence of charcoal in kiln sites did not affect total porosity. The water retention curve measurements revealed that water content was mostly affected in the mesopore range by the century-old charcoal content. This effect was strongest for the sandy loam. On the other hand, the presence of century-old charcoal increased the hydraulic conductivity at pF between 1.5 and 2 for the silt loam, while no effect of charcoal was observed for the loamy and sandy loam soils. Results are discussed with respect to biochar characteristics and the various ways in which biochar particles could be distributed within soils. Overall, the present study highlights a limited effect of century-old charcoal on the pore size distribution (at constant porosity) and on the resulting soil physical properties.