Results are presented from a study concerning the reduction in soil hydraul
ic conductivity due to ponded hog manure. Of specific interest is how much
of the reduction is 'at the soil surface' as opposed to within the soil. Se
ven different soils with clay contents ranging from 9 to 33% were studied u
sing 200 mm long soil columns in a low-temperature (5-6 degreesC) environme
nt. Hydraulic conductivities, as measured with water, ranged between 3.0 x
10(-8) and 1.3 x 10(-6) m/s before manure application. Fresh hog manure was
ponded on these soil columns for a period of 634 days. Hydraulic conductiv
ity, for all soils, decreased rapidly to about 1.0 x 10(-9) m/s and maintai
ned this value except during the time of failure of the cooling system. A b
lack layer was observed to have developed at the manure-soil interface of a
ll columns within 36 hours of manure pending. Visual observations conducted
between days 136 and 618 showed that the black layer grew downwards into t
he soil at a rate of 0.3 mm/month. The hydraulic conductivities of the soil
s at different depth intervals indicated that most, if not all, of the redu
ction occurred at the black surface layer. At the end of the 634 day period
, the black layer was removed and soil hydraulic conductivities were measur
ed once again using a prepared chemical solution of similar ionic concentra
tion to that of manure. The hydraulic conductivities of all soils increased
to that of 'pre-manure' conditions. The results of this study suggest that
the hydraulic conductivity reduction from ponded hog manure under these ex
perimental conditions is mainly related to the development of the black lay
er at the manure-soil interface.