EQUILIBRIUM OF HETEROGENEOUS SUBSTANCES.
207
under the most general supposition with respect to the position of the co-ordinate axes.
For any principal axis of strain we have
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when
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the differential coefficients in the first of these equations being determined from (420) as before. Therefore,
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(426)
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From (420) we obtain directly
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(427)
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From the two last equations, in virtue of the necessary relation
, we obtain
![{\displaystyle {\tfrac {1}{2}}{\frac {d(r^{2})}{d\alpha '}}=\alpha 'r^{2},}](https://wikimedia.org/api/rest_v1/media/math/render/svg/a2bb071b4c85a2fd6a294bafc0b5207c93dffb7a) ![{\displaystyle {\tfrac {1}{2}}{\frac {d(r^{2})}{d\beta '}}=\beta 'r^{2},}](https://wikimedia.org/api/rest_v1/media/math/render/svg/1d2ad08d2dd067b94e648119751b440e826c4787)
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(428)
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or, if we substitute the values of the differential coefficients taken from (420),
![{\displaystyle \alpha '\textstyle \sum \displaystyle \left({\frac {dx}{dx'}}\right)^{2}+\beta '\textstyle \sum \displaystyle \left({\frac {dx}{dx'}}{\frac {dx}{dy'}}\right)+\gamma '\textstyle \sum \displaystyle \left({\frac {dx}{dx'}}{\frac {dx}{dz'}}\right)=\alpha 'r^{2},}](https://wikimedia.org/api/rest_v1/media/math/render/svg/fcf02119daea7bca481234a3a9617423c868a4dd) |
(429)
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If we eliminate
from these equations, we may write the result in the form,
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(430)
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We may write
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(431)
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(432)
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