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Introduction
Irrigated agriculture has been essential in this century to provide
food and fiber for an expanding population. Production per unit
area of irrigated land will become more important in the future
if population continues to grow. Some estimates show that world
population has doubled in only 32 years and there is no indication
population growth will slow down. At the same time, the productivity
of many irrigation projects has been declining due to waterlogging,
salinity and poor irrigation management practices. The long-term
practice of intensive irrigation for cultivated areas has in many
cases transformed fertile land with high crop yields to salinized
soils with low fertility and reduced crop yields. Examples of the
effects of this practice include the Nile Valley in Egypt, the Tigris-
Euphrates Valley in Iraq and California's San Joaquin Valley in
the United States.
Irrigation alters the natural hydrological cycle in arid and semiarid
regions. After irrigation has been introduced the total water added
to soils often exceeds evapotranspiration (ET) and this causes increases
in the water table within the root zone. When the water evaporates,
water will move upward from the water table. At the same time plant
roots deplete water from the top soil causing an effect described
as a capillary rise of water from shallow groundwater sources. This
water can be used to supplement irrigated water. However, unless
the land is properly managed, capillary rise from saline groundwater
may cause the salinization of the soil. Salinization occurs when
water moves upward through the soil and the dissolved salts move
with it. Then, when the water evaporates from the soil surface or
is taken into the roots of a plant the salts remain behind in the
soil. Eventually, the salt build-up will cause decreased crop yields.
To solve the problem of salinization, additional irrigation water
needs to be added to leach the excess salts from the root zone and
drains must be installed to make a net downward movement of water.
Soluble salts increase or decrease in the root zone depending on
whether the net downward movements of salt is less or greater than
the net salt input from irrigation water and other sources.
Control of waterlogging and salinity in arid and semiarid regions
depends on integrated water management which includes irrigation,
leaching and drainage. Sustained long-term crop production in areas
with saline shallow water tables requires designing and managing
irrigation and drainage systems conjunctively. Decisions about irrigation
and drainage must take into account the consequent soil salinity
and waterlogging which affects crop yields over a season.
The rate of expansion of irrigated land reached a peak of 2.3 percent
per year from 1972 to 1975. It has declined since and is now less
than 1 percent per year. The decline in rate of expansion is due
to higher costs and lowered performance. Since projects that have
adequate drainage are much more efficient with higher performance
and lower costs, irrigated land can be improved for higher productivity
by designing irrigation and drainage systems conjunctively with
adequate modeling and considerations of all the parameters.
CSU-ID is a computer-based Decision Support System (DSS) for the
design and management of conjunctive irrigation and drainage systems.
The DSS can be used to improve the design and management of new
irrigation projects and it can be used for the rehabilitation of
existing projects. It will provide advanced technology to assist
professionals in analyzing field- scale irrigation and drainage
systems in semiarid and arid areas.
Software
Design
CSUID runs on a PC running Windows. The graphical user interface
(GUI) was developed using the "C" programming language
and "Motif" and "X Intrinsic Libraries" for
graphics. This GUI is based on a mouse driven approach that allows
the user to select the options from the program by pressing the
different mouse buttons (there are three mouse buttons on a Sun
Workstation mouse). With this user friendly interface, users are
freed from time-consuming tasks associated with analysis of numerical
output in the form of large output files, file input, and computer
program execution.
CSU-ID allows users to manipulate large amounts of spatial information
required to manage irrigation and drainage systems. The user can
study the spatial variability of data and the impacts of design
and management decisions on an irrigation and drainage systems.
CSU-ID significantly reduces the amount of effort involved in the
creation and/or debugging of a input data set, and improves the
understanding of the output.
Graphical
User Interface
The GUI for CSUID is a combination of window, menu, and icon selections
designed to allow movement quickly and easily through the model.
CSUID was written to run on a Sun SPARCstation and it has been ported
to a Data General UNIX workstation. The graphical user interface
(GUI) was developed using the "C" programming language
combined with OSF/Motif and Xt Intrinsic Libraries for the graphics.
It is based on a mouse driven approach with pull-down menus and
pop-up windows. The GUI makes tasks of data entry, editing, or viewing
easier and faster with the provision of editing tools that allows
the user to graphically specify the data. Different irrigation and
drainage scenarios (drain spacing, depth from the ground surface,
irrigation rate, irrigation duration, and irrigation frequency)
can be easily formulated for sensitivity analysis. Moreover, the
modular arrangement of the data allows the user to specify only
the part of the data that needs to be edited.
The main window of the interface is shown in Figure 1. There are
five pull-down menus in the menu bar along the top of the window.
These pull-down menus contain the major functions of CSUID including:
1) file, provides the user the ability to save and retrieve input
files in project directories, start new projects, and manage different
projects in different directories; 2) edit input, allows the user
to view all simulation data related to input for simulation parameters,
grid spacing, drain-collector connectivity, irrigation schedule,
and print controls; 3) view output, allows the user to view parameters
spatially and to select the output day for viewing results; 4) run,
allows the user to start the simulation program; and 5) help, a
hierarchical help facility describing in detail all the options
in the program.
The common options used in both editing input and viewing output
are provided along the left-hand side of the main window. These
options allow the user the ability to zoom into a particular area
on the grid, query a grid cell, view time series data, edit the
spatial input parameters, edit the boundaries, select locations
where time series data are requested, blink all the cells with the
same value, and show or remove grid lines. There are two additional
items in the common options for viewing output; they are, selection
of viewing axis (x-y, x-z, y-z) and display of all or selected boundaries
(natural boundaries, drains, collectors, and basins). A map scale
is provided in the main display where the spatial map is shown.
A message window near the bottom of the screen displays status information
about the program.
Irrigation
and Drainage Systems
Historically, most irrigation and drainage systems were designed
separately and the responsibility for the management of irrigation
and drainage systems has generally been assigned to different agencies.
But, the optimal use of irrigated agricultural lands requires irrigation
and drainage systems to be designed, constructed and managed as
an integrated unit. A combined system can be very complex, requiring
modeling to fully understand and predict long-term performance.
Irrigation practices have direct effects on the water table, drain
spacing is dependent on excess water applied and rainfall, and the
costs and benefits of irrigation and drainage need to be mutually
considered.
Modeling
Irrigation and Drainage Systems
Many of the variables affecting irrigation and drainage systems
are stochastic in nature. Irrigation scheduling is based on ET,
crop growth stage and available soil water. The stochastic nature
of meteorological variables can be simulated using a weather generator.
Generated meteorological time series can be used as input into the
scheduling model. The resulting stochastic schedules generated creates
uncertainty in the system behavior. Similarly, system boundary conditions,
soil flow and formation properties (hydraulic conductivity, pressure-saturation
characteristics, etc.), irrigation application efficiency and other
parameters can be modeled as cross-correlated spatial- temporal
random fields.
The
Numerical Model
The numerical model is a quasi-three dimension model used as the
basis for computing the spatial and temporal distributions of soil
water and salinity as affected by irrigation and drainage design
and management practices in the presence of a saline shallow water
table. The model solves the depth-averaged Boussinesq equation for
aerial flow in the saturated zone below the water table and the
Richard's equation for one-dimensional vertical flow in the unsaturated
zone above the water table. The mixing cell concept is used to predict
advection- dominated salinity transport. Solutions are obtained
via finite difference approximations of the equations at discrete
grid points in the domain. In addition to calculating salinity and
water distributions, the model predicts depth to the water table,
upward flux from the water table, leaching efficiency, volume and
salinity of drainage effluent collected, and relative crop yield.
The model explicitly considers variability due to the diverse soil
and crop properties and irrigation practices on multiple fields
in an area. Future enhancements will allow a fully stochastic option
where selected parameters (representing system boundary conditions
and properties) may be modeled as cross-correlated spatial-temporal
random fields.