The Sustainability of Floods Pond

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Transcription:

The Sustainability of Floods Pond Bangor Water District s Public Water Supply Presented By: Rick Pershken Bangor Water District

Overview Brief BWD History Watershed Characteristics Lake Characteristics Safe/Sustainable Yield Pumpage & Usage Records Precipitation Records Lake Levels

BWD History The Bangor Water District was formed in 1957 Prior to the formation of the Water District, water was supplied by the City of Bangor from a treatment plant located on the Penobscot River March 10, 1951 And while this water is somewhat less vile than that which Philadelphia drinks, it has a noticeable flavor of rotten sawdust and moose tracks.

BWD History Initially looked at ground water (Veazie) and surface water sources. Floods Pond in Otis was eventually selected. 1958 - Johnston Pump Station, 5 miles of road, overhead electric and 17 miles of transmission main were constructed for a cost of $4,000,000 (about 32.2 million today). 1995 Butler Water Treatment Facility Constructed ($8,000,000) 2013 UV Facility Constructed ($3,000,000)

Watershed Map Drainage Area 8.8 square miles (5,632 acres). Topography Hills and lakes, glacial scoured. Soils Glacial till based Dixfield- Colonel-Lyman- Brayton association. Land Use Forested, managed sustainably.

Watershed Characteristics Burnt Pond 326 acres, 33 feet deep Little Burnt Pond 10 acres 15 ephemeral and 1 perennial inlet streams Tannery Brook - outlet 1% Wetland Sand & Gravel Aquifers - none 98.7% Owned or Protective Agreement

Bedrock Lucerne Granite

Lake Characteristics Surface area 756 acres Maximum Depth 142 feet Spillway 305.5 feet, fixed crest Mean Depth 41 feet Usable Storage 4.5 billion gallons to elevation 282 Temperature 33.2 low, 74.5 High, 50.7 Avg. Quality Coldwater Lake high quality, oligotrophic Secchi Disk 23 to 26 feet/thermocline Biology Arctic Charr. Spawn at Kimball Point on shallow cobble shoal highly susceptible to water level fluctuations

Depth Map

Charr Sustainability Charr Management Plan (IF&W, BWD) Limit BWD withdrawal to 6 MGD (1990) Limit BWD withdrawal to 6.5 MGD (1991) Withdrawal limit no longer appropriate (1996) IF&W & BWD Joint management of Charr Employ range of alternatives to withdrawal limitations to ensure sustainability of the Charr. Annual monitoring of Charr population. Kimball Point Dec. 2001, Elev. 300 +/- October, 2009 Elev. 305 +/-

Elevation of Charr Spawning Beds

Safe/ Sustainable Yield Difficult to define. Safe yield is more of a maximum drought yield while sustainable yield may be more conservative as it considers maintaining baseflow. The use of the term safe yield is declining.

Regulations Chapter 587 In-stream Flows and Lake and Pond Water Levels (2007) establishes river and stream flows and lake and pond water levels to protect natural aquatic life and other designated uses in Maine 's waters Standard Allowable Alteration April 1 to July 31 (1 foot drawdown) August 1 to March 31 (2 foot drawdown) Public Water Utilities - these requirements will not apply to an existing Community Water System operating within its system design capacity providing that (1) the Community Water System, so operating, cannot attain the applicable requirements, and (2) the Community Water System has received, and is operating in accordance with, or is otherwise satisfying the requirements of, a Community Water System Withdrawal Certificate issued by the Department. A Community Water System Withdrawal Certificate will be issued by the Department to any existing Community Water System that demonstrates that it cannot operate at its system design capacity and attain the applicable flow or water level requirements of this chapter. There is also a drought flow variance for Community Water Systems

Safe Yield Black & Veatch (1989) Used a monthly water balance equation; Water In = Water Out +/- Changes in Storage Analyzed for period of March 1948 to February 1952 (2 nd driest period on record). Assumed a maximum of 23.5 foot drawdown Results 8.2 MGD safe yield.

Safe Yield Rule of Thumb 1 Square Mile = 1 MGD Average Yield in Maine (MGD) = DA (acres) * 43,560 ft2/acre * 7.48 gal/ft3* 0.5 (APT) / 365 days/year/1,000,000 DA = drainage area (acres) APT = average annual precipitation (feet) Floods Pond average annual yield = 8.8 MGD Drought Yield = 8.8 * 85% = 7.5 MGD 50% = 4.4 MGD The more conservative the more sustainable

Johnston Pump Station Two intakes: one 185 feet long at 292 feet (13.5 ); the other 302 feet long at 282.5 feet (23 ). Four 3,000 GPM x 150 HP, vertical turbine pumps Initial Maximum Design Capacity = 16 MGD. Current Design Capacity 13 MGD (limited by Ozone Treatment Plant 1995).

Water Pumped 6.00 5.50 5.57 Aug Summer Peaks 5.00 MGD PUMPED 4.50 4.00 Winter Lows 3.77 (Dec.) 3.50 3.00 Oct-97 Nov-99 Dec-01 Jan-04 Feb-06 Mar-08 Apr-10 May-12 Jun-14 Jul-16 DATE

Water Pumped as Percentage of Safe Yield (8.2 MGD) 100% 90% 80% 70% 68% 67% PERCENT OF SAFE YIELD 60% 50% 40% 30% 20% 10% 0% Jan-99 Jan-00 Jan-01 Jan-02 Jan-03 Jan-04 Jan-05 Jan-06 Jan-07 Jan-08 Jan-09 Jan-10 Jan-11 Jan-12 Jan-13 DATE

Pumped Vs. Metered Water Used 6.00 5.50 5.00 Water Pumped WATER USED (MGD) 4.50 4.00 3.50 Metered Water 3.00 2.50 2.00 2004 2005 2006 2007 2008 2009 2010 2011 2012 2013 YEAR

Unmetered/Unaccounted Water Unmetered - Hydrant & Main Flushing Standpipe Draining Process Water Fire Fighting Main Breaks Unaccounted for Leaks we don t know about Unauthorized use or unreported use Measurement inaccuracy

Precipitation Average annual precipitation = 42 8 drought periods in the record with the two worst occurring between 1947-1950 (Before use as PWS) and between 1999-2002. Drought What is It? 85% of average annual precipitation A period of below average water content in streams, reservoirs, ground water aquifers, lakes and soils. a deficit of precipitation sufficient to create stress on and competition for otherwise adequate drinking water supplies Schmitt 2003 Palmer drought severity index is negative 2.0 or less

Historical Precipitation 14.0 160% 12.0 140% MONTHLY PRECIPITATION (INCHES) 10.0 8.0 6.0 4.0 120% 100% 80% 60% 40% PERCENTAGE OF AVERAGE ANNUAL PRECIPITATION 2.0 20% 0.0 1/2/1991 1/2/1993 1/3/1995 1/3/1997 1/4/1999 1/4/2001 1/5/2003 1/5/2005 1/6/2007 1/6/2009 1/7/2011 1/7/2013 0%

Lake Levels Natural Outlet Level = 302.5 New dam lake level (1978) = 305.5 October, 2001 Level = 301 +/- Steve on the Dam Level = 306 +/- June, 2013

Low Lake Levels Floods Pond Lowest Annual Intake Level 306 305 spillway 304.9 304.6 304.3 304.8 304.5 304.3 305.07 304 303.5 303.6 303.3 303.7 303.69 Feet 303 302 302.5 outlet pipe 302.3 302.1 302.3 301.7 Natural charr beds 302.9 302.4 302.9 302.9 302.8 301 300 299 298 New Beds - Down to 292 300.5 300.2

Lake Levels 308.0 307.0 More Conservative = More Predictable? 306.0 Spillway Crest 305.0 LAKE LEVEL (FT) 304.0 303.0 8 Pipe Outlet 302.0 301.0 12/24/01 Record Ground Water Low in Closest USGS Bedrock Well Ground water/surface Water Interaction? 300.4 1/13/02 300.0 12/23/88 9/19/91 6/15/94 3/11/97 12/6/99 9/1/02 5/28/05 2/22/08 11/18/10 8/14/13 5/10/16 DATE

The Sustainability of Floods Pond Bangor Water District s Public Water Supply Presented By: Rick Pershken Bangor Water District

Partial List of References The Soils of Maine, John A. Ferwerd, Kenneth J. LaFlamme, Norman R. Kalloch, Jr., Natural Resources Conservation Service, USDA and Robert V. Rourke Department of Applied Ecology and Environmental Sciences, University of Maine. Geologic map of the Lucerne Granite, Hancock and Penobscot Counties, Maine Wones, D.R., and Ayuso, R.A. Publishing Organization: U.S. Geological Survey http://www.flyrodreel.com/magazine/2010/wither-maine-char SUSTAINABLE YIELD OF GROUNDWATER Victor M. Ponce May 2007 http://waterdata.usgs.gov/nwis Dina Page, Kathy Moriarty, Data, Photos, Advice. Bangor Water District THE EFFECTS OF THE 2001-2002 DROUGHT ON MAINE DRINKING WATER SUPPLIES, DRINKING WATER PROGRAM Department of Health & Human Services http://www.medwp.com Catherine Schmitt January 2005 Management Plan Landlocked Arctic Charr Floods Pond, Otis, Maine, 1996.