When the effect of groundwater level storage treatment without any salinity (W 0 S 0 , W 1 S 0 , and W 2 S 0 ) was analyzed, a clear trend in GI and VI was observed: dry storage (95.9% ± 3.6 and 85.9% ± 4.7%, respectively) > high groundwater level storage (49.3% ± 9.9 and 51.9% ± 7.1%) > low groundwater level storage (30.1% ± 9.3 and 35.7% ± 5.4%) ( Figure 4 ).
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Rising Shallow Groundwater Level May Facilitate Seed Persistence in the Supratidal Wetlands of the Yellow River Delta.
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