TY - JOUR
T1 - Overland flow generation and continuity on stone‐covered soil surfaces
AU - Lavee, H.
AU - Poesen, J. W.A.
PY - 1991
Y1 - 1991
N2 - The influence of stone cover on the generation and continuity of overland flow is a function of several variables, primarily stone size, distance (spacing) between stones, and stone position (on top of the soil surface or partially embedded). The initial hypothesis of the present study were that stone size affects overland flow generation by inducing ‘concentration overland flow’ and that the distance between stones affects overland flow continuity. With respect to stone size and distance between stones, opposing results have been found in the literature. Accordingly, the present paper reports on laboratory experiments which were conducted to investigate, systematically, the effect on overland flow of stone size, distance between stones, and stone position. The main conclusions were: Stone cover tended to induce overland flow, relative to bare soil. Small stones, however, especially in a low‐cover percentage setting, and when resting on top of the soil surface, produced less overland flow than bare soil. Overland flow was positively related to stone size, but inversely related to distance between stones. Overland flow yield was always greater when stones were embedded than when on top of the soil surface. The effect of stone size on increasing the degree of overland flow was of greater significance than the effect of the distance between stones on reducing overland flow.
AB - The influence of stone cover on the generation and continuity of overland flow is a function of several variables, primarily stone size, distance (spacing) between stones, and stone position (on top of the soil surface or partially embedded). The initial hypothesis of the present study were that stone size affects overland flow generation by inducing ‘concentration overland flow’ and that the distance between stones affects overland flow continuity. With respect to stone size and distance between stones, opposing results have been found in the literature. Accordingly, the present paper reports on laboratory experiments which were conducted to investigate, systematically, the effect on overland flow of stone size, distance between stones, and stone position. The main conclusions were: Stone cover tended to induce overland flow, relative to bare soil. Small stones, however, especially in a low‐cover percentage setting, and when resting on top of the soil surface, produced less overland flow than bare soil. Overland flow was positively related to stone size, but inversely related to distance between stones. Overland flow yield was always greater when stones were embedded than when on top of the soil surface. The effect of stone size on increasing the degree of overland flow was of greater significance than the effect of the distance between stones on reducing overland flow.
KW - Distance between stones
KW - Overland flow
KW - Stone cover
KW - Stone position
KW - Stone size
UR - http://www.scopus.com/inward/record.url?scp=0026359127&partnerID=8YFLogxK
U2 - 10.1002/hyp.3360050403
DO - 10.1002/hyp.3360050403
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AN - SCOPUS:0026359127
SN - 0885-6087
VL - 5
SP - 345
EP - 360
JO - Hydrological Processes
JF - Hydrological Processes
IS - 4
ER -