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The author induces a new mean value method to be most effectively applied to the continuous curve which intersects a horizontal axis at both ends of defined interval. According to this new method, some calculating formulas for discharge in natural streams are obtained. When we apply these formulas to stream gaging, the smallest number of the verticals, consequently of the measuring points, may be sufficient. Therefore, we can measure the most accurate value of discharge, because we can prolong the period of velocity measurement at every points to eliminate the effect of pulsations of moving water, and moreover the shortening of the total period of gaging makes the effect of changing stage as little as possible.

INDUCEMENT OF A NEW MEAN VALUE METHOD AND CALCULATING FORMULAS FOR DISCHARGE IN NATURAL STREAMS