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s with the convex curve marked with the difference between the wet and dry readings. The horizontal line passing through this intersection will give the relative humidity. Example: Dry bulb 70 deg., wet bulb 62 deg., difference 8 deg.. Find 70 deg. on the horizontal line of temperature. Follow up the vertical line from 70 deg. until it intersects with the convex curve marked 8 deg.. The horizontal line passing through this intersection shows the relative humidity to be 64 per cent. EXAMPLE 2. To find how much water per cubic foot is contained in the air: Find the relative humidity as in example 1. Then the nearest concave curve gives the weight of water in grains per cubic foot when the air is cooled to the dew-point. Using the same quantities as in example 1, this will be slightly more than 5 grains. EXAMPLE 3. To find the amount of water required to saturate air at a given temperature: Find on the top line (100 per cent humidity) the given temperature; the concave curve intersecting at or near this point gives the number of grains per cubic foot. (Interpolate, if great accuracy is desired.) EXAMPLE 4. To find the dew-point: Obtain the relative humidity as in example 1. Then follow up parallel to the nearest concave curve until the top horizontal (indicating 100 per cent relative humidity) is reached. The temperature on this horizontal line at the point reached will be the dew-point. Example: Dry bulb 70 deg., wet bulb 62 deg.. On the vertical line for 70 deg. find the intersection with the hygrometer (convex) curve for 8 deg.. This will be found at nearly 64 per cent relative humidity. Then follow up parallel with the vapor pressure (concave) curve marked 5 grains to its intersection at the top of the chart with the 100 per cent humidity line. This gives the dew-point as 57 deg.. EXAMPLE 5. To find the change in the relative humidity produced by a change in temperature: Example: The air at 70 deg. Fahr. is found to contain 64 per cent humidity; what will be its relative humidity if heated to 150 deg. Fahr.? Starting from the intersection of the designated humidity and temperature coordinates, follow the vapor-pressure curve (concave) until it intersects the 150 deg. temperature ordinate.
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