Assabet River NWR Final CCP - U.S. Fish and Wildlife Service

Assabet River NWR Final CCP - U.S. Fish and Wildlife Service Assabet River NWR Final CCP - U.S. Fish and Wildlife Service

23.12.2012 Views

- 20 - Chapter 3: Refuge and Resource Descriptions permeability. They tend to be droughty, with severe concern for seedling survival and slight concern for erosion in well managed forest cover. Windsor soils are found in nearly level to very steep conditions; are up to 5+ feet deep; excessively drained soils on glacial outwash plains, terraces, deltas and escarpments. They formed in sandy glacial outwash, and have a very friable or loose loamy sand or loamy fin sand surface soil. They have rapid permeability and tend to be droughty, but concern for seedling mortality is listed as being slight. Merrimac soils occur in level to steep slopes; are up to 5+ feet deep; and, are excessively drained soils found on glacial outwash plains, terraces, and kames. They formed in water-sorted, sandy glacial material, and are friable, fine sandy loams and sandy loams in the surface. They are moderately rapid in permeability, with few limitations for most uses, and moderate risk for seedling mortality. Paxton soils are deep (5+ feet), well drained soils found on glacial drumlins. They formed in compact glacial till. These soils are friable fine sandy loams, with a very stony surface. They have slow or very slow permeability and moderate risk for seedling mortality. The Deerfield series are deep, well drained, loamy fine sand soils. They are found on glacial outwash plains, terraces, and deltas. These soils may have a seasonal high water table at 18 to 36 inches and moderate seedling mortality risk. Montauk soils are well drained and found on drumlins. They formed in compact glacial tills, and are friable, fine sandy loams, with moderately rapid permeability. Montauk soils are stony to extremely stony, with a slight seedling mortality risk. The Charton-Hollis-rock outcrop complex soils are well drained, with (on average) approximately 10% bedrock outcrops. The Swansea and Freetown series are very poorly drained wetland soils. They formed in depressions and flat areas of glacial outwash plains and terraces, and may be 50 inches to many feet of black, highly decomposed organic material over sandy mineral materials. They have a water table that is at or near the surface most of the year (USDA 1995). Hydrology Most of the northern section and westernmost parts of the southern section of Assabet River NWR fall within the Assabet River drainage basin. The majority of the northern portion of the refuge drains northward through Taylor Brook and its tributaries, including Honey Brook. Two small, intermittent streams also flow from the northern/northwest portion of the Assabet River NWR

Chapter 3: Refuge and Resource Descriptions refuge into the Assabet River. The central and eastern areas of the southern portion of the refuge are within the Sudbury River drainage basin. Marlboro Brook drains from the southeastern portion of this section of the refuge into Hop Brook, a tributary of the Sudbury River, just above Stearns Millpond. The western portions of this section of the refuge drain toward White Pond, which has no surface outlet, but is thought to drain underground to Lake Boon and thence to the Assabet River (U.S. Army 1995). The water table under much of the refuge is shallow, as indicated by the extensive swamps, bogs, and water-holes found on the property. Groundwater discharge is thought to be supplying much of the flow occurring through the outwash plains underlying the lowlands of the site (U.S. Army 1995). The poorly drained lowlands soils have Taylor Brook: Photo by Marijke Holtrop supported the establishment of extensive and diverse wetland habitats, which include forested and shrubdominated wetlands, bogs, emergent wetlands, open-water bodies in the form of several lakes and ponds, an abandoned cranberry bog, and scattered seasonally-flooded vernal pools (USFWS 1995). Air Quality The Massachusetts annual air quality report for 1999 (MADEP, 2000), and the U.S. Environmental Protection Agency’s (USEPA) air quality planning and standards web page (EPA, 2001), contain the most recent data available for air quality in this area. The nearest data appear to be limited to those from monitoring sites in the City of Worcester and the Town of Stow. The Stow monitoring site has been located on the Assabet River NWR since 1999, and prior to that time was located nearby on the Great Meadows NWR in Sudbury. The pollutants for which state-wide data are available are ozone (O 3 ), carbon monoxide (CO), nitrogen dioxide (NO 2 ), lead (Pb), sulfur dioxide (SO 2 ) and particulate matter (both 2.5 microns (PM2.5) and 10 microns (PM10)). The National Ambient Air Quality Standards (NAAQS) determined by USEPA set the concentration limits that determine the attainment status for each criteria pollutant. Massachusetts does not attain the public health standard for two pollutants – ozone (O 3 ) for the entire state and CO in a few cities (MADEP 2000), including parts of Worcester and Middlesex counties within which the refuge is located (USEPA 2001). There are two ozone standards based on two different averaging times, 1hour and 8-hour. In 1999, there were 85 exceedances of the 8-hour standard occurring on 22 days, and 5 exceedances of the 1- hour standard occurring on 4 days on a state-wide basis. The 12-year trends for ozone readings in Comprehensive Conservation Plan - 21 -

Chapter 3: Refuge <strong>and</strong> Resource Descriptions<br />

refuge into the <strong>Assabet</strong> <strong>River</strong>. The central <strong>and</strong> eastern areas of the<br />

southern portion of the refuge are within the Sudbury <strong>River</strong> drainage<br />

basin. Marlboro Brook drains from the southeastern portion of this section<br />

of the refuge into Hop Brook, a tributary of the Sudbury <strong>River</strong>, just above<br />

Stearns Millpond. The western portions of this section of<br />

the refuge drain toward White Pond, which has no surface<br />

outlet, but is thought to drain underground to Lake Boon<br />

<strong>and</strong> thence to the <strong>Assabet</strong> <strong>River</strong> (U.S. Army 1995).<br />

The water table under much of the refuge is shallow, as<br />

indicated by the extensive swamps, bogs, <strong>and</strong> water-holes<br />

found on the property. Groundwater discharge is thought to<br />

be supplying much of the flow occurring through the<br />

outwash plains underlying the lowl<strong>and</strong>s of the site (U.S.<br />

Army 1995). The poorly drained lowl<strong>and</strong>s soils have<br />

Taylor Brook: Photo by Marijke Holtrop<br />

supported the establishment of extensive <strong>and</strong> diverse<br />

wetl<strong>and</strong> habitats, which include forested <strong>and</strong> shrubdominated<br />

wetl<strong>and</strong>s, bogs, emergent wetl<strong>and</strong>s, open-water bodies in the<br />

form of several lakes <strong>and</strong> ponds, an ab<strong>and</strong>oned cranberry bog, <strong>and</strong><br />

scattered seasonally-flooded vernal pools (USFWS 1995).<br />

Air Quality<br />

The Massachusetts annual air quality report for 1999 (MADEP, 2000), <strong>and</strong><br />

the U.S. Environmental Protection Agency’s (USEPA) air quality planning<br />

<strong>and</strong> st<strong>and</strong>ards web page (EPA, 2001), contain the most recent data<br />

available for air quality in this area. The nearest data appear to be limited<br />

to those from monitoring sites in the City of Worcester <strong>and</strong> the Town of<br />

Stow. The Stow monitoring site has been located on the <strong>Assabet</strong> <strong>River</strong><br />

<strong>NWR</strong> since 1999, <strong>and</strong> prior to that time was located nearby on the Great<br />

Meadows <strong>NWR</strong> in Sudbury.<br />

The pollutants for which state-wide data are available are ozone (O 3 ),<br />

carbon monoxide (CO), nitrogen dioxide (NO 2 ), lead (Pb), sulfur dioxide<br />

(SO 2 ) <strong>and</strong> particulate matter (both 2.5 microns (PM2.5) <strong>and</strong> 10 microns<br />

(PM10)).<br />

The National Ambient Air Quality St<strong>and</strong>ards (NAAQS) determined by<br />

USEPA set the concentration limits that determine the attainment status<br />

for each criteria pollutant. Massachusetts does not attain the public health<br />

st<strong>and</strong>ard for two pollutants – ozone (O 3 ) for the entire state <strong>and</strong> CO in a few<br />

cities (MADEP 2000), including parts of Worcester <strong>and</strong> Middlesex counties<br />

within which the refuge is located (USEPA 2001).<br />

There are two ozone st<strong>and</strong>ards based on two different averaging times, 1hour<br />

<strong>and</strong> 8-hour. In 1999, there were 85 exceedances of the 8-hour st<strong>and</strong>ard<br />

occurring on 22 days, <strong>and</strong> 5 exceedances of the 1- hour st<strong>and</strong>ard occurring<br />

on 4 days on a state-wide basis. The 12-year trends for ozone readings in<br />

Comprehensive Conservation Plan - 21 -

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