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In Constructing a Confidence Interval For σ\sigma Or σ2\sigma ^ { 2 }

question 29

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In constructing a confidence interval for σ\sigma or σ2\sigma ^ { 2 } , a table is used to find the critical values χL2\chi { } _ { L } ^ { 2 } and χR2\chi _ { \mathrm { R } } ^ { 2 } for values of n101\mathrm { n } \leq 101 . For larger values of n,χL2n , \chi _ { \mathrm { L } } ^ { 2 } and χR2\chi _ { \mathrm { R } } ^ { 2 } can be approximated by using the following formula: χ2=12[±zα/2+2k1]2\chi ^ { 2 } = \frac { 1 } { 2 } \left[ \pm \mathrm { z } _ { \alpha / 2 } + \sqrt { 2 \mathrm { k } - 1 } \right] ^ { 2 } where k\mathrm { k } is the number of degrees of freedom and zα/2\mathrm { z } _ { \alpha / 2 } is the critical z score. Estimate the critical values χL2\chi _ { \mathrm { L } } ^ { 2 } and χR2\chi _ { \mathrm { R } } ^ { 2 } for a situation in which you wish to construct a 95%95 \% confidence interval for σ\sigma and in which the sample size is n=295n = 295 .

Identify and explain the structural and functional aspects of hydrostatic skeletons and coelomates.
Identify and apply the rules for naming branched alkanes and their isomers.
Understand and describe the condensed structural formula representation of hydrocarbons.
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Definitions:

Contact Metamorphism

A type of metamorphism that occurs when rocks are heated by the intrusion of hot magma without melting.

Subduction

The process whereby one tectonic plate moves under another plate and is forced to sink into the mantle, often leading to volcanic activity and earthquakes.

Normal Faulting

A type of faulting where the crust is extended and the hanging wall moves down relative to the footwall.

Partly Metamorphic

Relating to rocks that have been partially altered in structure or composition by heat, pressure, or chemical processes.

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