Community Urbanization Science Fair Projects

Objectives/Goals

THIS PROJECT WAS CONDUCTED TO DETERMINE THE IMPACT THAT URBANIZATION HAS ON SYCAMORE CANYON CREEK IN THE CITY OF RIVERSIDE. IT WAS PREDICTED THAT THE CONCENTRATIONS OF ALKALINITY, CHLORIDE, DISSOLVED OXYGEN, ELECTRICAL CONDUCTIVITY, HARDNESS, NITRATE, pH, PHOSPHATE, SALINITY, AND TOTAL DISSOLVED SOLIDS (TDS) WOULD INCREASE IN DISTANCE THROUGH THE CITY.

Methods/Materials

IN ORDER TO CONDUCT THIS EXPERIMENT, TITRATION KITS, VACUETTE KITS, AND ELECTRODE METERS WERE USED. THE TITRATION KITS WERE USED TO DETERMINE ALKALINITY, CHLORIDE, AND SALINITY LEVELS. DISSOLVED OXYGEN, HARDNESS, NITRATE, AND PHOSPHATE LEVELS WERE FOUND VIA VACUETTE KITS. FINALLY, CONDUCTIVITY, pH, AND TDS WERE GATHERED BY THE ELECTRODE METERS. FOUR LOCATIONS ALONG SYCAMORE CANYON CREEK WERE USED AS TESTING SITES FROM WHICH WATER SAMPLES WERE COLLECTED. THESE SAMPLES WERE THEN TESTED AT HOME.

Results

FOR MOST OF THE ELEMENTS TESTED, THE TRENDS SHOWED THAT THE LEVELS INCREASED AS THE CREEK PROGRESSED DOWNSTREAM; HOWEVER, THE DATA OF SITE 4, INSIDE RIVERSIDE COMMUNITY COLLEGE, BROKE THE INCREASING TREND. PHOSPHATES, NITRATES, TDS, CONDUCTIVITY, AND ALKALINITY FOLLOWED THIS PATTERN. DISSOLVED OXYGEN, CHLORIDE, PH, AND HARDNESS, DID NOT FOLLOW A UNIQUE DEVELOPMENT AS THE CREEK PROGRESSED THROUGH RIVERSIDE. SALINITY WAS THE ONLY ELEMENT THAT FOLLOWED THE HYPOTHESIS, CONSTANTLY INCREASING FROM SITE TO SITE.

Conclusions/Discussion

BASED ON THE AVERAGE DATA FOR EACH OF THE COMPONENTS, THE HYPOTHESIS WAS DISPROVEN FOR ALL THE ELEMENTS TESTED, EXCEPT SALINITY. FOR THE MAJORITY OF THE WATER COMPONENTS, THERE WAS A LINEAR INCREASE FROM SITE 1 TO SITE 3; NONETHELESS, THE LEVEL SEEMED TO DROP AT SITE 4. RUNOFF FROM DIFFERENT SOURCES MIGHT HAVE DILUTED THE CONCENTRATIONS OF THE ELEMENTS, CAUSING THE DROP AT SITE 4. 3rd party contributor