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11/uJ vL L1~ l uu •.y~ u~v r... v.v. •~~ ""' <br />r <br />Addendum <br />Pa[: <br />Note that smaller water-table declines (less than 1 meter) in coarse flood plain alluvium (for <br />example gravels) would likely produce the same effects as reported here, since gravel and <br />cobbles would have much less plant-available water following water-table drawdown. This was <br />noted by Condra in 1944 (see discussion on page 356 of the paper). <br /> <br />