Description[Monitoring][Preliminary Results]
Field B is approximately 3km from Field A, sharing similar underlying geology of glacial sands and gravels overlying the Upper Chalk. The field is approximately 80ha and has a network of field drains, at approximately 30 m spacing, draining into a drainage ditch. The ditch is usually hydrologically active from October to March, for the remainder of the year the ditch is dry.
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