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  2. Plus–minus method - Wikipedia

    en.wikipedia.org/wiki/Plus–minus_method

    The plus–minus method, also known as CRM (conventional reciprocal method), is a geophysical method to analyze seismic refraction data developed by J. G. Hagedoorn. It can be used to calculate the depth and velocity variations of an undulating layer boundary for slope angles less than ~10°.

  3. Zeller's congruence - Wikipedia

    en.wikipedia.org/wiki/Zeller's_congruence

    These formulas are based on the observation that the day of the week progresses in a predictable manner based upon each subpart of that date. Each term within the formula is used to calculate the offset needed to obtain the correct day of the week. For the Gregorian calendar, the various parts of this formula can therefore be understood as follows:

  4. Haversine formula - Wikipedia

    en.wikipedia.org/wiki/Haversine_formula

    In that case, a and b are ⁠ π / 2 ⁠ − φ 1,2 (that is, the, co-latitudes), C is the longitude separation λ 2 − λ 1, and c is the desired ⁠ d / R ⁠. Noting that sin(⁠ π / 2 ⁠ − φ) = cos(φ), the haversine formula immediately follows. To derive the law of haversines, one starts with the spherical law of cosines:

  5. Weibull distribution - Wikipedia

    en.wikipedia.org/wiki/Weibull_distribution

    For k > 1, the density function tends to zero as x approaches zero from above, increases until its mode and decreases after it. The density function has infinite negative slope at x = 0 if 0 < k < 1, infinite positive slope at x = 0 if 1 < k < 2 and null slope at x = 0 if k > 2. For k = 1 the density has a finite negative slope at x = 0.

  6. Subtraction - Wikipedia

    en.wikipedia.org/wiki/Subtraction

    The minuend digits are m 3 = 7, m 2 = 0 and m 1 = 4. The subtrahend digits are s 3 = 5, s 2 = 1 and s 1 = 2. Beginning at the one's place, 4 is not less than 2 so the difference 2 is written down in the result's one's place. In the ten's place, 0 is less than 1, so the 0 is increased by 10, and the difference with 1, which is 9, is written down ...

  7. Schofield equation - Wikipedia

    en.wikipedia.org/wiki/Schofield_equation

    1.7: 1.6: Intense exercise lasting 20–45 minutes at least three time per week, or a job with a lot of walking, or a moderate intensity job. Very active 2.1 1.9 Intense exercise lasting at least an hour per day, or a heavy physical job, such as a mail carrier or an athlete in training. Extremely active 2.4 2.2

  8. Chemical formula - Wikipedia

    en.wikipedia.org/wiki/Chemical_formula

    An example of the difference is the empirical formula for glucose, which is CH 2 O (ratio 1:2:1), while its molecular formula is C 6 H 12 O 6 (number of atoms 6:12:6). For water, both formulae are H 2 O. A molecular formula provides more information about a molecule than its empirical formula, but is more difficult to establish.

  9. Plus–minus (sports) - Wikipedia

    en.wikipedia.org/wiki/Plus–minus_(sports)

    When a goal is scored by a team on the power play, no plus or minus points are awarded to either team. Empty net situations are treated the same as even-strength unless the team that scores is on the power play. [1] Penalty shot goals are excluded. A player's plus−minus statistic is calculated for each game played.

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