PRINCIPAL INVESTIGATOR
Gene E. Likens
Institute of Ecosystem Studies
OTHERS INVOLVED
see References
BEGIN DATE
June 1967
END DATE
On-going
LOCATION
Central buoy station on Mirror Lake
LOCATION DESCRIPTION
Collected in a boat from an anchored
buoy station, or from the ice surface located at the deepest part (11 m
at full pool) of Mirror Lake. Mirror Lake is 15 ha in area, and an oligotrophic
(low productivity), clearwater (Secchi transparency 6 to 7 m), natural
water body adjacent to HBEF. The lake normally mixes in spring and fall,
and is ice-covered from about 1 December to about 15 April each year. Numerous
studies have been conducted on Mirror Lake since the mid-1960s, including
extensive physical, chemical, biological, and paleoecological research
which are described in detail in the book: An Ecosystem Approach to Aquatic
Ecology (Likens, 1985).
DATA DESCRIPTION
Concentrations (mg/L) in lake
water samples from discrete depths. Base cation, pH, and dissolved oxygen
data are available since 1967. Ammonium, anions, phosphate, and dissolved
silica have been measured routinely since 1970, although some data are
available prior to these dates for each solute. Other standard data include
temperature and specific conductance at each depth. Prior to 1990, not
all records have complete solute arrays. Since 1990, dissolved in-organic
carbon (DIC) and acid neutralizing capacity (ANC; alkalinity) have also
been measured on a routine basis, although prior data do exist.
SAMPLING DESIGN
Samples for ion analysis are collected
in acid-washed, deionized water-rinsed, polyethylene bottles, using a manual
closure, plastic VanDorn collector bottle (before 1990), triggered at discrete
depths, or lifted to the surface through weighted vinyl tubing by peristaltic
pump (since 1990). DO and DIC samples are collected in standard glass BOD
bottles. Typically, water samples are taken from the surface (<0.5m),
and at depths of 2, 4, 6, 8, and 10 meters. The usual sampling interval
is 4 to 6 times each year, especially at times of maximum and minimum thermal
stratfication. Temperatures are determined by thermistor probe (Whitney, YSI, or Digisense Models).
REFERENCES
DATA LOCATION
Institute of Ecosystem Studies, Robert
S. Pierce Ecosystem Laboratory, Hubbard Brook Experimental Forest, W.Thornton,
NH
LAST UPDATED
April, 2001
CONTACT PERSON
Gene Likens
Institute of Ecosystem Studies
Millbrook, NY 12545
Telephone: (845) 677-5343
E-mail: LikensG@ecostudies.org
VARIABLES
Records: 1657 total samples in 4 separate
files
Columns: supplied with the following
headers:
ws - watershed
year - year
mo - month
dy - day
z - depth in meters
Ca - calcium concentration in mg/L
Mg - magnesium concentration in mg/L
K - potassium concentration in mg/L
Na - sodium concentration in mg/L
NH4 - ammonium concentration in mg/L
pH - pH
SO4 - sulfate concentration in mg/L
NO3 - nitrate concentration in mg/L
Cl - chloride concentration in mg/L
PO4 - phosphate concentration in mg/L (soluble-reactive phosphate)
SiO2 - silica concentration in mg/L (measured as silicate)
ANC - acid neutralizing capacity in meq/L
DIC - dissolved inorganic carbon in mmoles/L
DO - dissolved oyxgen in mg/L
TEMP - temperature in degrees C
SpCond - specific conductance corrected to 25C
CODES
Missing data are coded with -3.
Values of 0.0 (zero) are below the detection limit of analysis.
DATA FILE NAME(S)
Data were separated and downloaded
from spreadsheets onto 3 individual files to make handling and data checking
easier.
ASCII file names:
mlake-69.txt covering the period 1967 to 1969
264 records
mlake-79.txt covering the period 1970 to 1979
643 records
mlake-89.txt covering the period 1980 to 1989
516 records
mlake-95.txt covering the period 1990 to 1995
234 records