Hydrological Properties of a Clay Loam Soil as Affected by Biochar Application in a Pot Experiment

Improving soil‐water relations by amending soil with biochar might play a significant role in increasing water availability for agricultural crops as well as decreasing water loss through drain‐ age or runoff. While the effects of biochar on the hydrological properties on coarse‐textured soils are generally positive and well‐documented in the literature, studies on biochar effects on fine‐tex‐ tured soils are rather scarce and even contradictory. Therefore, the aim of this paper was to investi‐ gate the impact of biochar on the bulk density, water retention curve (together with several water capacitive indicators) and water infiltration rate in a clay loam soil. A pot experiment was carried out under lab conditions in which biochar was mixed with soil at rates of 0 (B0 or control), 2, 4, 6, 8 and 10% dw (B2, B4, B6, B8 and B10, respectively). Water retention of soil–biochar mixtures at dif‐ ferent matrix potentials was determined using a pressure plate apparatus. From these measure‐ ments, a series of capacitive indicators was derived and the fitting of the van Genuchten model was also performed. Water infiltration into soil–biochar mixtures was measured by means of a mini‐ disk infiltrometer and the obtained data were analyzed both directly and by fitting the Philip’s model. Biochar significantly affected the considered soil properties. As the biochar rate increased, the bulk density decreased and water retention increased (B6, B8 and B10 > B2, B4 and B0), while the infiltration rate decreased (B0 > B2, B4, B6, B8 and B10). Although the experiment was performed on sieved and repacked soil samples under lab conditions, the results confirmed that biochar has the potential to increase plant‐available water, while possibly reducing drainage water in a clay loam soil by lowering the infiltration rate.