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Demonstration Lysimeter

Model No. HD 10.1

With the HD 10.1 equipment, it is a question of knowing the water retention capacity of a soil using the hydrological balance, differentiating each one of its elements.

By means of the simulation of a rain on a soil, the following elements of the hydrological cycle are distinguished:
– Surface runoff: Once the soil is flooded, surface runoff begins, collecting it externally and proceeding to its measurement by evaluating its quantity in volume.
– Subsurface and subterranean runoff: The infiltrated water is collected by the bottom of the container, measuring this runoff by its volume.
– The rest of the water is absorbed by the soil that can be known by performing a weighing of the same before the rain and another after.
– The difference corresponds to the volume of stored water.
– By establishing the equality of volumes, the values of surface runoff, ground runoff and soil runoff are known.
– The equipment has a digital balance on which the floor model is set, so that the weight variation can be continuously displayed.

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