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(C) The rate of transpiration is inversely proportional to atmospheric pressure. When atmospheric pressure is low,such as at high altitudes,the air de

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Increase

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(C) The rate of transpiration is inversely proportional to atmospheric pressure. When atmospheric pressure is low,such as at high altitudes,the air density decreases,which facilitates the diffusion of water vapor from the leaf surface into the surrounding atmosphere. Therefore,the rate of transpiration increases.

Due to low atmospheric pressure,the rate of transpiration will

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