Hydrology and Runoff

Horton's infiltration equation expresses infiltration capacity $f_p$ at time $t$ as:

Options:

• (A) $f_p = f_c + (f_0 - f_c) e^{-kt}$
• (B) $f_p = f_0 + (f_c - f_0) e^{kt}$
• (C) $f_p = f_c \cdot t^{-k}$
• (D) $f_p = f_0 - k t$