FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1486563323> ?p ?o ?g. }

• W1486563323 abstract "OF THESIS Hydrologic Modeling to Examine Land Use Change Impacts (1970’s and 2005) on the Sediment Yield and Flow regime in Cayuga Creek, Niagara County, New York ABSTRACTThis research aims to assess the water quality and the land use change impacts on sediment concentration and flow regime in Cayuga Creek, Niagara County, NY for two land use periods, 1970’s and 2005. The 1970’s land use, classified by the USGS, had a significant error. Therefore, the scenario of sediment yield and discharge level to land use change is more of a “what if” since the 1970’s land use was classified incorrectly. The Soil and Water Assessment Tool (SWAT)was used to simulate flows and sediment concentrations for the two land use scenarios using the same rainfall data at the upstream and downstream sites. The modeling results indicated that the discharges at the downstream site were higher than those at the upstream site for both 1970’s and 2005 land uses. The sediment concentration was higher at the downstream site than the upstream site for 1970’s land use and the result was in an opposite direction for 2005 land use. Hydrolab Datasonde 4a’s were installed at an upstream and downstream site for a ten week period in order to assess water quality. The parameters monitored were: dissolved oxygen, pH, conductivity, turbidity, and temperature. Grab samples were taken in order to examine total suspended solids levels and establish a relationship with turbidity. This research aims to assess the water quality and the land use change impacts on sediment concentration and flow regime in Cayuga Creek, Niagara County, NY for two land use periods, 1970’s and 2005. The 1970’s land use, classified by the USGS, had a significant error. Therefore, the scenario of sediment yield and discharge level to land use change is more of a “what if” since the 1970’s land use was classified incorrectly. The Soil and Water Assessment Tool (SWAT)was used to simulate flows and sediment concentrations for the two land use scenarios using the same rainfall data at the upstream and downstream sites. The modeling results indicated that the discharges at the downstream site were higher than those at the upstream site for both 1970’s and 2005 land uses. The sediment concentration was higher at the downstream site than the upstream site for 1970’s land use and the result was in an opposite direction for 2005 land use. Hydrolab Datasonde 4a’s were installed at an upstream and downstream site for a ten week period in order to assess water quality. The parameters monitored were: dissolved oxygen, pH, conductivity, turbidity, and temperature. Grab samples were taken in order to examine total suspended solids levels and establish a relationship with turbidity. Kimly Reth August, 2012 State University of New York College at Buffalo Hydrologic Modeling to Examine Land Use Change Impacts (1970’s and 2005) on the Sediment Yield and Flow Regime in Cayuga Creek, Niagara County, New York A Thesis in Multidisciplinary Studies By Kimly Reth Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science August 2012" @default.
• W1486563323 created "2016-06-24" @default.
• W1486563323 creator A5047447503 @default.
• W1486563323 date "2012-01-01" @default.
• W1486563323 modified "2023-09-26" @default.
• W1486563323 title "Hydrologic Modeling to Examine Land Use Change Impacts (1970’s and 2005) on the Sediment Yield and Flow Regime in Cayuga Creek, Niagara County, New York" @default.
• W1486563323 cites W124402982 @default.
• W1486563323 cites W127139594 @default.
• W1486563323 cites W1482700787 @default.
• W1486563323 cites W1493200868 @default.
• W1486563323 cites W1524444317 @default.
• W1486563323 cites W1529526237 @default.
• W1486563323 cites W1536340909 @default.
• W1486563323 cites W1545235613 @default.
• W1486563323 cites W1573350472 @default.
• W1486563323 cites W1575788992 @default.
• W1486563323 cites W1592537543 @default.
• W1486563323 cites W1596061762 @default.
• W1486563323 cites W1601510412 @default.
• W1486563323 cites W1629642785 @default.
• W1486563323 cites W169461928 @default.
• W1486563323 cites W1728792544 @default.
• W1486563323 cites W1751136839 @default.
• W1486563323 cites W1839261311 @default.
• W1486563323 cites W1887863118 @default.
• W1486563323 cites W1964109019 @default.
• W1486563323 cites W1970571200 @default.
• W1486563323 cites W1980127305 @default.
• W1486563323 cites W1983724666 @default.
• W1486563323 cites W1985167980 @default.
• W1486563323 cites W1989556826 @default.
• W1486563323 cites W2000084913 @default.
• W1486563323 cites W2001508722 @default.
• W1486563323 cites W2002847057 @default.
• W1486563323 cites W2008501065 @default.
• W1486563323 cites W2009080666 @default.
• W1486563323 cites W2010738418 @default.
• W1486563323 cites W2010871948 @default.
• W1486563323 cites W2011695476 @default.
• W1486563323 cites W2011796652 @default.
• W1486563323 cites W2015273163 @default.
• W1486563323 cites W2020866710 @default.
• W1486563323 cites W2021851541 @default.
• W1486563323 cites W2024400993 @default.
• W1486563323 cites W2025329525 @default.
• W1486563323 cites W2027580577 @default.
• W1486563323 cites W2028548314 @default.
• W1486563323 cites W2029543544 @default.
• W1486563323 cites W2031438999 @default.
• W1486563323 cites W2031606396 @default.
• W1486563323 cites W2037583293 @default.
• W1486563323 cites W2042681318 @default.
• W1486563323 cites W2045109097 @default.
• W1486563323 cites W2049606884 @default.
• W1486563323 cites W2052438628 @default.
• W1486563323 cites W2054660155 @default.
• W1486563323 cites W2056456276 @default.
• W1486563323 cites W2056481894 @default.
• W1486563323 cites W2060009955 @default.
• W1486563323 cites W2062062852 @default.
• W1486563323 cites W2064124738 @default.
• W1486563323 cites W2065115059 @default.
• W1486563323 cites W2069607036 @default.
• W1486563323 cites W2077038928 @default.
• W1486563323 cites W2077440336 @default.
• W1486563323 cites W2087069004 @default.
• W1486563323 cites W2092721200 @default.
• W1486563323 cites W2094209997 @default.
• W1486563323 cites W2099648436 @default.
• W1486563323 cites W2103477713 @default.
• W1486563323 cites W2121630447 @default.
• W1486563323 cites W2126569949 @default.
• W1486563323 cites W2132474903 @default.
• W1486563323 cites W2147105669 @default.
• W1486563323 cites W2147406638 @default.
• W1486563323 cites W2185696386 @default.
• W1486563323 cites W2280514005 @default.
• W1486563323 cites W2304361154 @default.
• W1486563323 cites W2315996648 @default.
• W1486563323 cites W2319208713 @default.
• W1486563323 cites W2323901892 @default.
• W1486563323 cites W2340793798 @default.
• W1486563323 cites W2467466614 @default.
• W1486563323 cites W2521493960 @default.
• W1486563323 cites W2523430092 @default.
• W1486563323 cites W265194661 @default.
• W1486563323 cites W269750265 @default.
• W1486563323 cites W2772878191 @default.
• W1486563323 cites W278887394 @default.
• W1486563323 cites W2796653788 @default.
• W1486563323 cites W3102498655 @default.
• W1486563323 cites W3134777831 @default.
• W1486563323 cites W3138601583 @default.
• W1486563323 cites W3212230143 @default.
• W1486563323 cites W568092464 @default.
• W1486563323 cites W580392308 @default.
• W1486563323 cites W2120246384 @default.
• W1486563323 hasPublicationYear "2012" @default.
• W1486563323 type Work @default.
• W1486563323 sameAs 1486563323 @default.

• next