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Geohydrology and Limnology of Walden Pond, Concord, Massachusetts

Water-Resources Investigations Report 01-4137

By John A. Colman and Paul J. Friesz

ABSTRACT

The trophic ecology and ground-water contributing area of Walden Pond, in Concord and Lincoln, Mass., were investigated by the U.S. Geological Survey in cooperation with the Massachusetts Department of Environmental Management from April 1997 to July 2000. Bathymetric investigation indicated that Walden Pond (24.88 hectares), a glacial kettle-hole lake with no surface inlet or outlet, has three deep areas. The maximum depth (30.5 meters) essentially was unchanged from measurements made by Henry David Thoreau in 1846. The groundwater contributing area (621,000 square meters) to Walden Pond was determined from water-table contours in areas of stratified glacial deposits and from land-surface contours in areas of bedrock highs. Walden Pond is a flow-through lake: Walden Pond gains water from the aquifer along its eastern perimeter and loses water to the aquifer along its western perimeter. Walden Pond contributing area also includes Goose Pond and its contributing area. A water budget calculated for Walden Pond, expressed as depth of water over the lake surface, indicated that 45 percent of the inflow to the lake was from precipitation (1.215 meters per year) and 55 percent from ground water (1.47 meters per year). The groundwater inflow estimate was based on the average of two different approaches including an isotope mass-balance approach. Evaporation accounted for 26 percent of the outflow from the lake (0.71 meters per year) whereas lake-water seepage to the groundwater system contributed 74 percent of the outflow (1.97 meters per year). The water-residence time of Walden Pond is approximately 5 years.

Potential point sources of nutrients to ground water, the Concord municipal landfill and a trailer park, were determined to be outside the Walden Pond groundwater contributing area. A third source, the septic leach field for the Walden Pond State Reservation facilities, was within the groundwater contributing area. Nutrient budgets for the lake indicated that nitrogen inputs (858 kilograms per year) were dominated (30 percent) by plume water from the septic leach field and, possibly, by swimmers (34 percent). Phosphorus inputs (32 kilograms per year) were dominated by atmospheric dry deposition, background ground water, and estimated swimmer inputs. Swimmer inputs may represent more than 50 percent of the phosphorus load during the summer.

The septic-system plume did not contribute phosphorus, but increased the nitrogen to phosphorus ratio for inputs from 41 to 59, on an atom-to-atom basis. The ratio of nitrogen to phosphorus in input loads and within the lake indicated algal growth would be strongly phosphorus limited. Nitrogen supply in excess of plant requirements may mitigate against nitrogen fixing organisms including undesirable blooms of cyanobacteria. Based on areal nutrient loading, Walden Pond is a mesotrophic lake. Hypolimnetic oxygen demand of Walden Pond has increased since a profile was measured in 1939. Currently (1999), the entire hypolimnion of Walden Pond becomes devoid of dissolved oxygen before fall turnover in late November; whereas historical data indicated dissolved oxygen likely remained in the hypolimnion during 1939. The complete depletion of dissolved oxygen likely causes release of phosphorus from the sediments. Walden Pond contains a large population of the deep-growing benthic macro alga Nitella, which has been hypothesized to promote water clarity in other clear-water lakes by sequestering nutrients and keeping large areas of the sediment surface oxygenated. Loss of Nitella populations in other lakes has correlated with a decline in water quality. Although the Nitella standing crop is large in Walden Pond, Nitella still appears to be controlled by nutrient availability. Decreasing phosphorus inputs to Walden Pond, by amounts under anthropogenic control would likely contribute to the stability of the Nitella population in the metalimnion, may reverse oxygen depletion in the hypolimnion, and decrease recycling of phosphorus from the sediments.

 

Contents

 

Abstract

Introduction

Geologic Setting and Bathymetry

Hydrology

Data-Collection Methods

Water-Table Configuration and Extent of the Ground-Water Contributing Area

Ground-Water and Lake-Stage Fluctuations

Water Balance

Precipitation and Evaporation

Ground-Water Inflow

Contributing-Area Approach

Isotope Mass-Balance Approach

Average Ground-Water Inflow

Water-Balance Results

Limnology

External Inputs

Ground-Water Nutrient Inputs

Sampling and Analytical Methods for Ground Water

Geochemical Conditions in the Aquifer

Ground-Water Point Sources

Ground-Water Background Source

Atmospheric Deposition Source

Swimmer Source

Other Nutrient Sources

Nutrient Limitation, Ratios, Source Size, Timing, and Disposal Strategies

Nutrient Loading Trophic Index

Plant Growth and Internal Cycling of Chemical Constituents

Methods of Sampling and Analysis of the Water Column

Temperature Stratification

Phytoplankton, Nitella, and Light

Dissolved Oxygen

Dissolved Oxygen in the Epilimnion

Dissolved Oxygen in the Metalimnion

Dissolved Oxygen in the Hypolimnion

Conductance, pH, Phosphorus, Nitrogen, Iron, Manganese, and Internal Nutrient Recycling

Historical, and Between-Lake Trophic Assessments

Trophic State from Water-Column Assessment

Historical Dissolved-Oxygen Profiles

Comparisons of Dissolved Oxygen Among Lakes

Trophic Stability

Trophic Ecology and Management Options

Summary and Conclusions

References Cited

Appendix A. Delta deuterium and delta oxygen-18 of lake water, ground-water inflow, and precipitation,Walden Pond

 


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Cover (82 KB)  - 1 page

Inside cover (19 KB) -2 pages

Contents (106 KB) - 3 pages

Body of Report    (8 MB) - 61 pages


U.S. Department of the Interior, U.S. Geological Survey
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Last modified: Wednesday, August 31 2005, 04:51:42 PM
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