series (redirected from erythrocytic series)

series, in mathematics, indicated sum of a sequence of terms. A series may be finite or infinite. A finite series contains a definite number of terms whose sum can be found by various methods. An infinite series is a sum of infinitely many terms, e.g., the infinite series 1-2 + 1-4 + 1-8 + 1-16 + … . The dots mean that the remaining terms are formed according to the rule made evident by the first few terms, in this case doubling the denominator of the preceding term to form that of the next term; the nth term of this series is ( 1-2)ⁿ. Some infinite series converge to a certain value called its limit; i.e., as one adds together progressively more terms, these sums (called the partial sums of the series) form a sequence of values that progressively approach the limit. For example, the series given above converges to the value 1 because the partial sums form the sequence 1-2, 3-4, 7-8, 15-16, … . Many series, however, do not converge, i.e., have no value that their partial sums approach. Such a series is 1-2 + 1-3 + 1-4 + … , for even though the terms become very small, enough of them added together will give a value greater than any number that can be named. A series that does not converge is said to diverge; various tests exist for determining whether or not a given series converges and for determining its limit if it does converge. See also progression.

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series

1. Maths the sum of a finite or infinite sequence of numbers or quantities

2. Electronics

a. a configuration of two or more components connected in a circuit so that the same current flows in turn through each of them (esp in the phrase in series)

b. (as modifier): a series circuit

3. Geology a stratigraphical unit that is a subdivision of a system and represents the rocks formed during an epoch

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series [′sir·ēz]

(analytical chemistry)

A group of results of repeated analyses completed by using a single analytical method on samples of a homogeneous substance.

(electricity)

An arrangement of circuit components end to end to form a single path for current.

(geology)

A number of rocks, minerals, or fossils that can be arranged in a natural sequence due to certain characteristics, such as succession, composition, or occurrence.

A time-stratigraphic unit, below system and above stage, composed of rocks formed during an epoch of geologic time.

(mathematics)

An expression of the formx₁+x₂+x₃+ ⋯, wherex_iare real or complex numbers.

(spectroscopy)

A collection of spectral lines of an atom or ion for a set of transitions, with the same selection rules, to a single final state; often the frequencies have the general formula [R/(a+c₁)²] - [R/(n+c₂)²], whereRis the Rydberg constant for the atom,aandc₁andc₂are constants, andntakes on the values of the integers greater thanafor the various lines in the series.