introduction flow, water-level, and water-quality monitoring · monitoring streamflow, water...

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0 1 2 3 4 5 6 7 8 9 10 Stage (feet) 0 1 2 3 4 5 6 7 8 9 10 Stage (feet) 11-15-2011 12-02-2011 12-19-2011 1-05-2012 1-22-2012 2-08-2012 2-25-2012 3-13-2012 3-30-2012 4-16-2012 5-03-2012 0 1 2 3 4 5 6 7 8 9 10 Stage (feet) Data from U.S. Geological Survey Ayers Creek at NE North Valley Road, near Gaston, OR (14202550) Wapato Canal at Pumphouse, at Gaston, OR (14202630) Wapato Creek at Gaston Rd at Gaston, OR (14202650) U.S. Department of the Interior U.S. Geological Survey November 2014 Most of the USGS monitors collected data from September 2011 to April 2013; the lake water-level gage is still deployed. Data from the telemetered sites can be viewed and explored online using the USGS Data Grapher website at: http://or.water.usgs.gov/cgi-bin/grapher/graph_setup.pl?basin_id=tualatin Data from the lake water-level gage also are available from the USGS National Water Information System website at: http://waterdata.usgs.gov/or/nwis/uv?site_no=14202630 The Data Grapher website allows users to interactively explore the available data, creating customized graphs and tables of various types, including comparisons of data from multiple sites, such as the graphs shown below. Streamflow was measured at the Ayers Creek site by measuring the water level with a pressure sensor, then converting that measurement to streamflow through a stage-discharge relation determined from flow measurements collected over a wide range of conditions. Streamflow at the Wapato Creek outflow site was measured with an acoustic velocity meter that used sound waves to measure the velocity of water; the velocity data combined with water-level data were used to calculate streamflow. The water-level sensors at various sites used underwater pressure sensors to measure the water depth. Water quality at the Wapato Creek outflow site was measured with an instrument equiped with seven different probes. The probes were maintained and calibrated every 3-4 weeks, year-round, to keep them operating properly. Wapato Lake near Gaston in northwestern Oregon has been a productive resource for fish, wildlife, and human populations for hundreds of years. Historically, seasonal high flows in the upper Tualatin River filled the lowland area comprising Wapato Lake. In the 1930s, a network of levees and canals was constructed to minimize seasonal flooding, facilitate the drainage of the lake in springtime for farming during summer, and convey water during summer to farmland in and around the lakebed. To augment tributary inflows during the summer dry season, a diversion canal from the Tualatin River to the Wapato Lake canal system was constructed to bring water around the lake to adjacent agricultural lands. Since the construction of the levees, streams that previously flowed into Wapato Lake no longer do so, leaving rainfall, groundwater seepage, and leakage through the levees as the only hydrologic inputs to the lakebed. Recently, the U.S. Fish and Wildlife Service (USFWS) purchased most of the lakebed inside the leveed area, with the goal of managing the area for birds, fish, and other wildlife as the Wapato Lake National Wildlife Refuge. To optimize the future management of the lakebed, a variety of data were collected to provide a better understanding of the hydrology of the area and the quality of the water moving through the system. In partnership with the USFWS, the U.S. Geological Survey (USGS) began monitoring streamflow, water levels, and water quality in the Wapato Lake area in September of 2011. Two streamflow gages, four water-level gages, and one water- quality station continuously collected data at key sites upstream, within, and downstream of the lake (see locations on map) through April of 2013. Several times each day, the data were transfered via satellite to the USGS database and made available to the public from USGS websites. One water-level gage is still operating today, providing real-time information on the amount of water in the lake. The streamflow and water-level stations collected data that are being used to better understand the hydrology of the system and quantify its water budget. In combination with high-resolution topographic data collected by USFWS, the data were used to construct a water-budgeting spreadsheet tool that predicts flows and water levels under future management scenarios. The water-quality station measured water temperature, pH, conductance, dissolved oxygen, turbidity, chlorophyll, and blue-green algae levels at the outlet of the lake, providing important information on the quality of the lake and canal water as well as the water exported downstream to the Tualatin River. Introduction View of Wapato Lake from the pumphouse taken July 19, 2008 (top) and April 13, 2010 (bottom). Photographs by Stewart Rounds and Micelis Doyle, USGS. Flow, Water-Level, and Water-Quality Monitoring Photos of Wapato Lake water-level monitor (top) and Wapato Creek water-quality monitor (bottom) by Micelis Doyle, USGS, September 30, 2011. View of control on Wapato Creek outflow canal (top) and the inner canal near the pumphouse (bottom). Photographs by Norman Buccola, USGS, June 29, 2011. Map of the Wapato Lake area, showing the locations of USGS streamflow, water- level, and water-quallity monitoring stations upstream of, within, and downstream of the historic lakebed. The levee around the lakebed is marked with a yellow line. Data from the water-level stations on Wapato Creek upstream of the lakebed, Hill Creek upstream of the lakebed, and the Tualatin River diversion canal are collected manually, while data from the Ayers Creek streamflow gage, the pumphouse water- level gage, and the Wapato Creek outlet water-quality monitor were telemetered. (Map modified from U.S. Fish and Wildlife Service.) Monitoring Streamflow, Water Levels, and Water Quality in the Wapato Lake National Wildlife Refuge, Oregon streamflow gage and water-quality monitor and water-level monitor streamflow gage streamflow gage water-level monitor water-quality monitor with streamflow gage water-level monitor water-level monitor water-level monitor USGS Monitoring Stations 0 1 2 3 4 5 6 7 8 9 10 11 Stage (feet) 2-15-2012 2-22-2012 2-29-2012 3-07-2012 3-14-2012 3-21-2012 3-28-2012 4-04-2012 4-11-2012 4-18-2012 4-25-2012 5-02-2012 5-09-2012 5-16-2012 5.0 5.2 5.4 5.6 5.8 6.0 6.2 6.4 6.6 6.8 7.0 7.2 pH Wapato Canal at Pumphouse, at Gaston, OR (14202630) Data from U.S. Geological Survey Wapato Creek at Gaston Rd at Gaston, OR (14202650) 0.0 0.5 1.0 1.5 2.0 2.5 3.0 3.5 4.0 4.5 5.0 5.5 6.0 6.5 7.0 7.5 Stage (feet) 2-15-2012 2-22-2012 2-29-2012 3-07-2012 3-14-2012 3-21-2012 3-28-2012 4-04-2012 4-11-2012 4-18-2012 4-25-2012 5-02-2012 5-09-2012 5-16-2012 0 10 20 30 40 50 60 70 80 90 100 110 120 130 140 150 Turbidity (FNU) Wapato Canal at Pumphouse, at Gaston, OR (14202630) Data from U.S. Geological Survey Wapato Creek at Gaston Rd at Gaston, OR (14202650) 0 1 2 3 4 5 6 7 8 9 10 Stage (feet) 11-15-2011 12-02-2011 12-19-2011 1-05-2012 1-22-2012 2-08-2012 2-25-2012 3-13-2012 3-30-2012 4-16-2012 5-03-2012 -200 -150 -100 -50 0 50 100 150 200 250 300 Discharge (ft 3 /s) Wapato Creek at Gaston Rd at Gaston, OR (14202650) Data from U.S. Geological Survey 0 1 2 3 4 5 6 7 Stage (feet) 2-15-2012 2-22-2012 2-29-2012 3-07-2012 3-14-2012 3-21-2012 3-28-2012 4-04-2012 4-11-2012 4-18-2012 4-25-2012 5-02-2012 5-09-2012 5-16-2012 50 100 150 200 250 300 350 400 Specific Conductance (µS/cm) Wapato Canal at Pumphouse, at Gaston, OR (14202630) Data from U.S. Geological Survey Wapato Creek at Gaston Rd at Gaston, OR (14202650) Water level (stage) data from three sites are plotted in the graph to the left, showing that a series of storms increased the flow in the creeks and caused the lake to accumulate about 4 feet of water. Flow and water-level data in the graph to the right show that rainfall often caused the Tualatin River to rise faster than Wapato Creek, causing water to flow upstream (negative discharge) for a short period of time. USGS data from spring of 2012 show interesting patterns when Wapato Lake was being pumped dry. Stage data in red show the water level in the lake, while water- quality data from a site downstream in blue show that the pumped water had higher conductance, lower pH, and low turbidity compared to water outside the levees. Contact: Stewart A. Rounds, USGS [email protected] 503-251-3280 staff plate to read water level

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Data from U.S. Geological Survey

Ayers Creek at NE North Valley Road, near Gaston, OR (14202550)Wapato Canal at Pumphouse, at Gaston, OR (14202630)Wapato Creek at Gaston Rd at Gaston, OR (14202650)

Thu Nov 8 20:53:41 2012

U.S. Department of the InteriorU.S. Geological Survey

November 2014

Most of the USGS monitors collected data from September 2011 to April 2013; the lake water-level gage is still deployed. Data from the telemetered sites can be viewed and explored online using the USGS Data Grapher website at: http://or.water.usgs.gov/cgi-bin/grapher/graph_setup.pl?basin_id=tualatin Data from the lake water-level gage also are available from the USGS National Water Information System website at: http://waterdata.usgs.gov/or/nwis/uv?site_no=14202630

The Data Grapher website allows users to interactively explore the available data, creating customized graphs and tables of various types, including comparisons of data from multiple sites, such as the graphs shown below.

Streamflow was measured at the Ayers Creek site by measuring the water level with a pressure sensor, then converting that measurement to streamflow through a stage-discharge relation determined from flow measurements collected over a wide range of conditions. Streamflow at the Wapato Creek outflow site was measured with an acoustic velocity meter that used sound waves to measure the velocity of water; the velocity data combined with water-level data were used to calculate streamflow. The water-level sensors at various sites used underwater pressure sensors to measure the water depth.

Water quality at the Wapato Creek outflow site was measured with an instrument equiped with seven different probes. The probes were maintained and calibrated every 3-4 weeks, year-round, to keep them operating properly.

Wapato Lake near Gaston in northwestern Oregon has been a productive resource for fish, wildlife, and human populations for hundreds of years. Historically, seasonal high flows in the upper Tualatin River filled the lowland area comprising Wapato Lake. In the 1930s, a network of levees and canals was constructed to minimize seasonal flooding, facilitate the drainage of the lake in springtime for farming during summer, and convey water during summer to farmland in and around the lakebed. To augment tributary inflows during the summer dry season, a diversion canal from the Tualatin River to the Wapato Lake canal system was constructed to bring water around the lake to adjacent agricultural lands. Since the construction of the levees, streams that previously flowed into Wapato Lake no longer do so, leaving rainfall, groundwater seepage, and leakage through the levees as the only hydrologic inputs to the lakebed.

Recently, the U.S. Fish and Wildlife Service (USFWS) purchased most of the lakebed inside the leveed area, with the goal of managing the area for birds, fish, and other wildlife as the Wapato Lake National Wildlife Refuge. To optimize the future management of the lakebed, a variety of data were collected to provide a better understanding of the hydrology of the area and the quality of the water moving through the system.

In partnership with the USFWS, the U.S. Geological Survey (USGS) began monitoring streamflow, water levels, and water quality in the Wapato Lake area in September of 2011. Two streamflow gages, four water-level gages, and one water-quality station continuously collected data at key sites upstream, within, and downstream of the lake (see locations on map) through April of 2013. Several times each day, the data were transfered via satellite to the USGS database and made available to the public from USGS websites. One water-level gage is still operating today, providing real-time information on the amount of water in the lake.

The streamflow and water-level stations collected data that are being used to better understand the hydrology of the system and quantify its water budget. In combination with high-resolution topographic data collected by USFWS, the data were used to construct a water-budgeting spreadsheet tool that predicts flows and water levels under future management scenarios.

The water-quality station measured water temperature, pH, conductance, dissolved oxygen, turbidity, chlorophyll, and blue-green algae levels at the outlet of the lake, providing important information on the quality of the lake and canal water as well as the water exported downstream to the Tualatin River.

Introduction

View of Wapato Lake from the pumphouse taken July 19, 2008 (top) and April 13, 2010 (bottom). Photographs by Stewart Rounds and Micelis Doyle, USGS.

Flow, Water-Level, and Water-Quality Monitoring

Photos of Wapato Lake water-level monitor (top) and Wapato Creek water-quality monitor (bottom) by Micelis Doyle, USGS, September 30, 2011.

View of control on Wapato Creek outflow canal (top) and the inner canal near the pumphouse (bottom). Photographs by Norman Buccola, USGS, June 29, 2011.

Map of the Wapato Lake area, showing the locations of USGS streamflow, water-level, and water-quallity monitoring stations upstream of, within, and downstream of the historic lakebed. The levee around the lakebed is marked with a yellow line. Data from the water-level stations on Wapato Creek upstream of the lakebed, Hill Creek upstream of the lakebed, and the Tualatin River diversion canal are collected manually, while data from the Ayers Creek streamflow gage, the pumphouse water-level gage, and the Wapato Creek outlet water-quality monitor were telemetered. (Map modified from U.S. Fish and Wildlife Service.)

Monitoring Streamflow, Water Levels, and Water Quality in the Wapato Lake National Wildlife Refuge, Oregon

streamflow gage and water-quality monitor

and water-level monitor

streamflow gage

streamflow gagewater-level monitor

water-quality monitor with streamflow gage

water-level monitor

water-level monitor

water-level monitor

USGS Monitoring Stations

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Wapato Canal at Pumphouse, at Gaston, OR (14202630)Data from U.S. Geological Survey

Wapato Creek at Gaston Rd at Gaston, OR (14202650)

Thu Nov 8 21:05:38 2012

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Wapato Canal at Pumphouse, at Gaston, OR (14202630)Data from U.S. Geological Survey

Wapato Creek at Gaston Rd at Gaston, OR (14202650)

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Wapato Creek at Gaston Rd at Gaston, OR (14202650)Data from U.S. Geological Survey

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Wapato Canal at Pumphouse, at Gaston, OR (14202630)Data from U.S. Geological Survey

Wapato Creek at Gaston Rd at Gaston, OR (14202650)

Thu Nov 8 21:03:06 2012

Water level (stage) data from three sites are plotted in the graph to the left, showing that a series of storms increased the flow in the creeks and caused the lake to accumulate about 4 feet of water.

Flow and water-level data in the graph to the right show that rainfall often caused the Tualatin River to rise faster than Wapato Creek, causing water to flow upstream (negative discharge) for a short period of time.

USGS data from spring of 2012 show interesting patterns when Wapato Lake was being pumped dry. Stage data in red show the water level in the lake, while water-quality data from a site downstream in blue show that the pumped water had higher conductance, lower pH, and low turbidity compared to water outside the levees.

Contact: Stewart A. Rounds, USGS [email protected]

503-251-3280

staff plate to read water level