Seepage (S) from animal-waste lagoons was estimated using a water balance a
pproach by measuring changes in waste level (i.e., depth) (Delta D) and eva
poration (E) over brief periods (e.g., 6 days) when all other inflow and ou
tflow were precluded. Data were collected at commercial swine and cattle fe
edlots in southwestern Kansas. Precision waste level recorders, floating ev
aporation pans, and meteorological models were used to measure each lagoon'
s water balance. Different strategies for calculating evaporation and seepa
ge were compared. Initial work at a 2.5-ha plastic-lined lagoon (S = 0, E a
pproximate to 5.1 mm d(-1)) showed that evaporation over 6- to 11-day perio
ds could be measured to within +/-0.5 mm d(-1) with floating evaporation pa
ns using a pan coefficient of 0.81. A bulk-transfer evaporation model, whic
h incorporated real-time measurements of lagoon surface temperature, predic
ted evaporation to within 6% when using a transfer coefficient of 2.8 x 10(
-3). Evaporation models that did not include surface temperature resulted i
n significant errors (e.g, > 50%) under certain environmental conditions. T
he water balance of a soil-lined, cattle-feedlot lagoon over an II-day peri
od was: do = 2.1; E = 1.9, and S = 0.2, all in mm d(-1). Additional work ov
er a 6-day period at a soil-lined, swine-waste lagoon resulted in a water b
alance of: Delta D = 5.4; E = 4.5, and S = 0.9, all in mm d(-1). Data sugge
st that seepage from lagoons can be determined to within +/-0.5 mm d(-1) by
making precision water balance measurements over short periods (5 to 10 da
ys), if evaporation is less than 6 mm d(-1).