The irrigated area in the Aral Sea basin totals about 7. 5 million
hectare. Part of the water supplied to this area is consumed by the
irrigated crop; the remainder of the supplied water drains to the
groundwater basin, to downstream depressions, or back to the rivers.
During its use, however, this drained part of the water accumulates
salts and chemicals. The disposal of this polluted water causes a
variety of (environmental) problems. If the percentage consumed water of
the total water supply to an irrigated area (the so-called overall
consumed ratio) can be increased, less water needs to be drained. This
alleviates part of the related (environmental) problems. Further, if the
overall consumed ratio for the above 7. 5 million hectare is improved,
less water needs to be diverted from the rivers. Hence, more water can
flow towards the Aral Sea. As mentioned above, part of the non-consumed
irrigation water drains to the groundwater basin. Commonly, the natural
discharge capacity of this basin is insufficient to handle this imported
water. As a result, the groundwater table rises towards the land surface
causing waterlogging. In (semi-)arid zones this waterlogging triggers a
soil salinity problem resulting to a significant reduction in crop
yields. The artificial increase of the discharge capacity, and lowering
of the groundwater table, solves the soil salinity problem.