WATER RESOURCES DATA FOR WASHINGTON 2003 51
Radioisotopes are isotopic forms of elements that exhibit
radioactivity. Isotopes are varieties of a chemical element
that differ in atomic weight but are very nearly alike in
chemical properties. The difference arises because the
atoms of the isotopic forms of an element differ in the
number of neutrons in the nucleus; for example, ordinary
chlorine is a mixture of isotopes having atomic weights of
35 and 37, and the natural mixture has an atomic weight
of about 35.453. Many of the elements similarly exist as
mixtures of isotopes, and a great many new isotopes have
been produced in the operation of nuclear devices such as
the cyclotron. There are 275 isotopes of the 81 stable
elements, in addition to more than 800 radioactive
isotopes.
Reach, as used in this report, is a length of stream that is
chosen to represent a uniform set of physical, chemical,
and biological conditions within a segment. It is the
principal sampling unit for collecting physical, chemical,
and biological data.
Recoverable from bed (bottom) material is the amount of
a given constituent that is in solution after a representative
sample of bottom material has been digested by a method
(usually using an acid or mixture of acids) that results in
dissolution of readily soluble substances. Complete
dissolution of all bottom material is not achieved by the
digestion treatment and thus the determination represents
less than the total amount (that is, less than 95 percent) of
the constituent in the sample. To achieve comparability of
analytical data, equivalent digestion procedures would be
required of all laboratories performing such analyses
because different digestion procedures are likely to
produce different analytical results. (See also “Bed
material”)
Recurrence interval, also referred to as return period, is the
average time, usually expressed in years, between
occurrences of hydrologic events of a specified type (such
as exceedances of a specified high flow or nonexceedance
of a specified low flow). The terms “return period” and
“recurrence interval” do not imply regular cyclic
occurrence. The actual times between occurrences vary
randomly, with most of the times being less than the
average and a few being substantially greater than the
average. For example, the 100-year flood is the flow rate
that is exceeded by the annual maximum peak flow at
intervals whose average length is 100 years (that is, once
in 100 years, on average); almost two-thirds of all
exceedances of the 100-year flood occur less than 100
years after the previous exceedance, half occur less than
70 years after the previous exceedance, and about one-
eighth occur more than 200 years after the previous
exceedance. Similarly, the 7-day, 10-year low flow (7Q
10
)
is the flow rate below which the annual minimum
7-day-mean flow dips at intervals whose average length is
10 years (that is, once in 10 years, on average); almost
two-thirds of the nonexceedances of the 7Q
10
occur less
than 10 years after the previous nonexceedance, half occur
less than 7 years after, and about one-eighth occur more
than 20 years after the previous nonexceedance. The
recurrence interval for annual events is the reciprocal of
the annual probability of occurrence. Thus, the 100-year
flood has a 1-percent chance of being exceeded by the
maximum peak flow in any year, and there is a
10-percent chance in any year that the annual minimum
7-day-mean flow will be less than the 7Q
10
.
Replicate samples are a group of samples collected in a
manner such that the samples are thought to be essentially
identical in composition.
Return period (See “Recurrence interval”)
Riffle, as used in this report, is a shallow part of the stream
where water flows swiftly over completely or partially
submerged obstructions to produce surface agitation.
River mileage is the curvilinear distance, in miles,
measured upstream from the mouth along the meandering
path of a stream channel in accordance with Bulletin No.
14 (October 1968) of the Water Resources Council and
typically is used to denote location along a river.
Run, as used in this report, is a relatively shallow part of a
stream with moderate velocity and little or no surface
turbulence.
Runoff is the quantity of water that is discharged (“runs
off”) from a drainage basin during a given time period.
Runoff data may be presented as volumes in acre-feet, as
mean discharges per unit of drainage area in cubic feet per
second per square mile, or as depths of water on the
drainage basin in inches. (See also “Annual runoff”)
Sea level, as used in this report, refers to one of the two
commonly used national vertical datums (NGVD 1929 or
NAVD 1988). See separate entries for definitions of these
datums.
Sediment is solid material that originates mostly from
disintegrated rocks; when transported by, suspended in, or
deposited from water, it is referred to as “fluvial
sediment.” Sediment includes chemical and biochemical
precipitates and decomposed organic material, such as
humus. The quantity, characteristics, and cause of the
occurrence of sediment in streams are affected by
environmental and land-use factors. Some major factors
are topography, soil characteristics, land cover, and depth
and intensity of precipitation.