Monthly diel monitoring studies for phosphorus content were conducted (1995
-1996 period) for multiple stations on Incline Creek, a mountain stream in
the Lake Tahoe basin (California-Nevada). Large discharge and particulate P
(PP) concentration fluctuations occurred during June in the early evening
as snowmelt from higher elevations arrived at the lower stream reaches. Jun
e diel dissolved organic P (DOP) concentrations steadily increased, while s
oluble reactive P (SRP) concentrations remained constant. June diel PP conc
entrations associated with sand-sized particles (PPsand: >63 mu m) exhibite
d a clockwise hysteresis, indicating possible sediment source depletion on
a daily timescale. June diel PP associated with silt- and clay-sized partic
les (PPsc: >0.45 mu m and <63 mu m) exhibited counterclockwise hysteresis b
ehavior, suggesting a potential groundwater contribution to PPsc. PPsc comp
rised the majority of PP concentration, except during high-discharge events
when PPsand, concentration was dominant. Areal PP loading, specifically PP
sand, appears to originate primarily from the lower eastern branch of Incli
ne Creek during the spring snowmelt season. Possible sources include a ski
resort/parking lot and a golf course. DOP and SRP areal loads were greatest
from the undeveloped upper subwatershed, suggesting that natural factors s
uch as slope are influencing loading of small-sized P fractions.