← Back to article

Equation 14 · Radioactive Clocks: How Nuclear Physics Gave Evolution Its Time

What does this equation mean?

N87/N86N_{87}/N_{86}

Read the formula alongside the article passage below. Each part has a deeper page with its role in the equation, the supporting passage and nearby citations.

This mathematical expression combines the displayed quantities; its precise role follows from the surrounding article text. Read the equation part by part below; each part has a contextual explanation and a link to its mathematical background.

Read it piece by piece

N87N_{87}

Symbol N_87

N8N_87 is a part of this expression. Its role is fixed by the surrounding article and by the operations shown in the formula.

Understand this part →

N86N_{86}

Symbol N_86

each mineral’s measured rubidium-87 to strontium-86 ratio [ 18 ].

Understand this part →

subscript

subscript

The lower label selects a particular version, component, or indexed member of the quantity. For example, x₀ and xₜ can be values at different positions.

Understand this part →

How to interpret it

Read this expression with the definitions, units, and assumptions supplied by the article.

What the article says around this equation

where RtR_t is each mineral’s measured present-day strontium-87 to strontium-86 ratio, R0R_0 is the shared initial ratio recovered as the line’s intercept, and N87N_{87}/N86N_{86} is each mineral’s measured rubidium-87 to strontium-86 ratio [ 18 ] . The initial composition is no longer an assumption fed into the calculation; it is an output the data themselves supply, and a poor fit to a straight line is itself a warning that the minerals did not, in fact, share a common origin or have remained closed systems since.

Read the equation in its article →

Sources cited in the surrounding passage

These citations give research context. Read each source to check which claims it supports.

Return to Radioactive Clocks: How Nuclear Physics Gave Evolution Its Time

See this formula across 1 published context →

Browse the mathematical compendium →