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Download SaltModM (modern) Download SaltMod (classic) |
Hints A version called SaltModM with a modernized user interface for the input replaces the classic version. In June 2020 it was considered necessary to provide the modernized SaltModM version with the option to pause the calculations each year so that input changes (for example the seasonal rainfall) can be made annually. Another version has been made, called SaltModMY, with the possibility to include in the input menu the seasonal irrigation, rainfall, runoff, surface drainage and agricultural data for all years over which the model is instructed to run. The yearly pause for manual input changes is then not required. This version van be made available on request. but it can also be downloaded from this address. On 6 October 2012, thanks to comments made by Jason Keller and Jacob Scherberg, a simpler version of SaltMod was introduced by the name of SaltCalc. It lacks the crop rotation and farmers' response options, but it permits the calculation of daily, weekly or monthly instead of seasonal water and salt balances in the soil. |
The manual contains the principles, theory, user
manual and examples of applications. It can be
found directly as
PDF
document or on the articles
page from where it can also be downloaded.
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In SaltMod there are various soil layers including the
rootzone and aquifer. There can be subareas with different irrigation intensity, as well as fallow land. Reuse of drainage water and water pumped up from the wells form part of the model. |
The salinity of the transition zone in this case appears to reduce in each season and in every year, but after year 11 it will come to an equilibrium. |
The capillary rise into the transition zone of the
unirrigated land starts in year 5. Thereafter, in season 2, it remains constant at 40 mm per season. In season 1 the capillary rise continues to increase up to year 21, whereafter it reduces. The reason for the reduction may be that irrigated land is being abandoned due to salinization so that to flow of percolation losses to the unirrigated land reduces and the capillary rise follows suit. |
Intially the watertable is quite deep, but due to the
introduction of irrigation, it starts rising, to reach
an equilibrium after year 7. In season 1, which is the irrigation seaon, the water table after year 7 is shallower than in season 2. |