Rhoades J.D.
in
Bouchet R. (ed.).
Reuse of low quality water for irrigation Bari : CIHEAM
Options Méditerranéennes : Série A. Séminaires Méditerranéens; n. 1 1989
pages 133-139
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--- Rhoades J.D . Eviden ce of th e poten tial u se of salin e water for irrigation . In : Bouchet R. (ed.).
Reuse of low quality water for irrigation. Bari : CIHEAM, 1989. p. 133-139 (Options Méditerranéennes : Série A. Séminaires Méditerranéens; n. 1)
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I Evidence of the potential I
use of saline water for irrigation
I James
Riverside Salinity Laboratory- UC Riverside - USA
in irrigated agriculture can occur in the near future because the readily available suitable lands and waters are fully developed ( U N World Food Conference, 1974). This author believes that this' conclusion is not entirely valid and that the
concept of suitability has been misapplied because of the conservative standurds used to assess the f i t n e s s o f w a t e r ( a n d l a n d ) f o r i r r i g a t i o n . Furthermore, only conventional criteria and procedures of producing crops under irrigation
have been considered in the evaluation of our future production capacity. Water commonly c l a s s i f i e d a s u n s u i t a b l e f o r i r r i g a t i o n b y c o n v e n t i o n a l m e t h o d s c a n o f t e n b e u s e d
successfully to grow crops without hazardous long- term consequences to crops or soils, even with the use of ordinary farming practices. The adoption of new croplwater management strategies will
further enhance the agricultural use of saline be expanded considerably through the implementation of certain strategies which allow greater use of more saline waters for irrigation. Considerable saline water, including drainage waters from irrigation projects and frequently associated shallow ground
waters, is available in many parts of the world, including the U S ,
Australia, and the
l n this paper, l present a n appropriate method for assessing the suitability of saline waters for irrigation, a brief review of relevant literature documenting the successful use of saline waters for irrigation, and the concept and summary results of a test of a new croplwater management strategy to facilitate the use of saline water for irrigation.
- Assessing the suitability of saline water for irrigation
The suitability of a
be evaluated on the basis of the specific conditions of use,
assessing the suitability of of:
1. composition
of the soil
2. of how
how
would of
1972).
A model
which uses
1976). A of it, called "watsuit", has also been developed and used to
- a of "watsuit"
(1987).
A of
1984). is accomplished using Table 1 and Figure 1, a s discussed
of
compositions A soil salinity
options
is deemed likely if the
of the
of will a yield
is a change in
in place of t h e no-
yield-loss of
by
(1977) (1986).
Example data given
in Figure 2.
The effect of of
(Le.
exists) is
uptake-weighted salinity" F, values of Table 1.
salinity F, values of Table 1
1 9 7 6 of changing the
index of of
To assess toxicity
specific used in
place of is used as
of
of t h e
topsoil of
- EC of 1982
details). The of the
is taken be t h a t of
of the soil at depth in the soil is if
of (1977) (1981).
Figure 1 can be used in lieu of Table 1
of conventional it
levels, of
be
of Table l of high of Table 1 Figure 1
is following example. Given
= 2 dSm-1 and a of 0.10 with conventional
salinity at steady-state is ECe = (1.88) (2) =
1.88 is
(F,) Table l.
to be is wheat with a
EC, of dSm-1 (Figure 2), t h e
is of
salinity is but 3.8 dSm-l. is
assess) s p e c i f i c s o l u t e as in the soil when they of
the effects of exchangeable sodium on by high
independently of soil
of a n
excessive ECiw
and The values in Figure estimates of the
soils. is
the
-
ECi, combinationof Figure 3.
The slope of is below
values of 10 ECi, axis at a value of 0.3 because of the dominating effect of at such low s a l i n i t i e s . T h u s , e v e n a t l o w l e v e l s o f
soil of salt
subsequently used effects, techniques.
Toxicity seldom
they should be assessed as 1987).
- Evidence of the potential of using saline waters for irrigation
of
have concluded 1977) that the bulk of
in the US as well) have
potential value of
would of
disposal and as well.
options
Though of on the successful use of
conventional schemes of will
allow, can be of
of 1,500 mg/L of total dissolved solids and up
to 5,000 mg/L Valley,
1976). et al. (1978)
to 7.1 dSm-1 without effects on yield. gives a of examples of
of of
of up to 6,000 mg/L often classed as acceptable and indeed used.
(1966) concluded that the the salinity level of a n
is (1978)
4,000 mg/L without
(1975) (1978)
that cotton is
of 4.6
dSm-1. tJha yields of alfalfa
achieved in the with 12,500 mg/L of
good
of 5,000-6,000 mg/L total dissolved solids.
cited above, the successful use of of up to about dSm-1 (-6,000 mg/L) was noted. been claimed that
be 1967;
1977);
(1976) the
use of to 15 dSm-1
annual monsoons. et al. (1952) with salinities of up to 20,000 mg/L in the
only when a
stand establishment. These
be often
the
combined with indicate of
as suitable can be used finding implies that if a of the UN
Food
of
suitability if
a would
- A crop/water
management strategy to facilitate the use of saline.watex-s
forirrigation
this section, a
of using is
of
et
al., 1988a, b). The impetus its
will if access to of salinity is available, unless significant losses in
signifcant changes of
The which meets
is to substitute the saline (such
the "good"
when they a suitably salt- stage; the "good" is used at
soil salinity in the use of
is used only a of the time. The timing and amount of substitution will
quality of the two
salt buildup in the
is alleviated in the subsequent
when a is
using the low-salinity
should be noted that a soil will not
become of a
a of a not
options
of
used to leach salts out of the seed and shallow soil depths. Subsequent "in season"
down in the ahead
of the advancing the
soil which
will be used a
This cyclic use of lllow't and "high" salinity
of a
a (50%) of the
This has i n a 20-
which was begun on a
a of
of wheat and of the melons.
Alamo
of The
a block of
two of cotton (a followed
by and
then by alfalfa (a
of cotton
with the wheat only
was used. was hypothesized that wheat would
d e s a l i n a t i o n of
alfalfa to of yield.
The yields of the in the successive -and block - given in Tables 2 and
No significant losses in the yields of
cycle of
(even CA
65-75%)
establishment. The mean yield of cantaloupe seed obtained in the CA
statistically significant. The yields of
melons of of cantaloupe
obtained by
in the Ca and CA in the C
Table 2).
cantaloupes using of wheat The yields of
Table
lint yield of
when it
A). no significant loss in lint yield in the second cotton use of
following seedling establishment which was accomplished
CA). But was a significant and substantial loss of lint yield, a s expected,
used
A). This loss of yield was caused by a loss of stand that in the second
in the seedbed No loss in yield of
in the block the
of
The qualities of all of
or on the i t
et al., 1988a).
of
and given
i n Tables 4 a n d 5
-
a n dblock - data include
data show that substantial amounts of
of loss.
The estimated amounts of by the as deep given i n T a b l e 6 by individual
by succession of
was assumed that consumptive use was the no substantial losses of
leaching.
on soil
et al., 198813).
of the when the
of the facilitate the use of
- Blending drainage waters for reuse or discharge
is not uncommon to to expand by
too saline use by
to obtain a of the mixed
t h a t is blending is
1 9 8 8 ~ ) . T h e following logic is applied. A plant
must (that would
used to
a saline (low osmotic potential) soil solution.
When a of
is mixed with a low-salinity
"good of the mix made up of the excessively
is left. is still as unusable
of view) as it was
point without excessive yield loss. Thus, a of the low-salinity (fully
as a consequence of blending.
Thus diluting excessively less
of
is only usable by
indicated that, any succession of of
of high salinity) available is
by:
EC, 1 -
ECb
EC
a, and the efficiencies needed a
of EC = 1.0 dSm-1, of
1/45 to 1/15 would be the most salt- With such effkiencies, 67% of
the most sensitive would
the most of such saline
to a common t h a t
supply of sensitive
The above estimate of of
is based on the assumption of steady-state conditions and use
of of
will not be of
sequentially with it. a is so saline that its
use is
diluting it with
of of the same or
in this of mixing, simply mixed the usable which must be by the plant. The
if the two used cyclically as
show that a loss i n of a
a good 1 9 8 8 ~ ) .
options
V - Conclusion and summary
of now
conventional methods of
of good of low salinity
of low
typically classified a s good
documents the successful use that can be made of
of of
of
be enhanced if a modified dual of management is used. The objective is to substitute the saline
of
yield loss
or
For
low
The feasibility of by
J.W. Wadleigh, 1952. Salt
of
salinization J., No. 44, pp. 307-310.
1979. The use of saline in
the Joint Commission on Scientific and Technical
L., 1966. of
to of
No. 10, pp. 185-189.
1967. Sci.
(31, pp. 89-96.
1976. of highly saline
conditions in soil a cyclic
Lubbock: Texas Tech. Aug. 1976, pp.
608-609.
Espstein, E.
A feasibility :Sci., No. 197, pp. 247-261.
~.
and 1975.
Chemical soil
cotton -
Symp., pp. 175-183.
A., 1976.
conditions. Salinity
Tech. Aug.
1976,pp.165-169.
Stolzy, 1978. Use of
(51, pp. 169-192.
and
i t s effect on the soil and on cotton fields.
No. 58, pp. 963-976.
E.V. and G.J. salt
Evaluation of existing data. Salinity Lubbock TexasTech. Aug. 1976, pp. 187-198.
E.V., 1986. of plants.
1 ( l ) , pp. 12-26.
-
1977. Valley of
C.O., 8 0 p.
J. and J.V.
the Valley of West Texas. 2 Salinity
Lubbock: Texas Tech.
Aug. 1976,pp. 339-344.
evaluating the effective salinity and sodicity of
Salinity Lubbock Texas Tech.
Aug. 1976, pp. 1-14.
X.J., 1972. with saline New 198p.
A.F. and Salinity
and management in No.
pp.
Quality of for Soil Sci., No. pp.
for using
for Water
and Nevada, July
pp.
for
a to salt loading of
lnt'l Symp., State-of-the-Art Control Salinity. Utah: Salt Lake City, July
for
America. Venezuela, Oct. pp.
Also published in Scientific review on arid zone, Vol. :
New for using
for Spec.
Conference, Water Today and Tomorrow, July Flagstaff, AZ.
Use of for
Nat'l
Water Quality Bulletin, No. pp.
of for
supplies. Agri.
and Assessing the
suitability of for
of Salinity and Alkalinity. FAO Soil
J. Letey, G.J. W .J. Alves, Swain,
and of drainage water for
irrigation Hilgardia (in
F.T. J. Letey,
W.J. A1ves;G.J. J.A.
Swain and 1988b. o f drainage water
for irrigation: Soil
balance. Hilgardin (in Shalhevet, J. and J.
salinity: a l n t 7 C o m m i s s i o n o n p.
and sodium of estimating of soil or Soil Sci. Soc.
Ameri. J., No. pp.
UN Food Assessment ofthe World
Nov.
options méditerranéennes
Table 1: Relative concentration or electrical conductivity of soil water (saturation paste extract basis) at steady-state compared to that of irrigation water (Fc)
Rootzone interval 0.05 0.1 o 0.20 0.30 0.40 0.50
- - - _ _ _ _ _ - - _ _ _ _ _ - - _ - _ _ - _ _ _ _ _ _ _ _ _ _ _ _ - - - _ - - _ - _ - _ _ _
Linear average (1)
Upper quarter 0.65 0.64 O. 62 0.60 , 0.58 0.56
Whole rootzone 2.79 1.88 1.29 1 .O3 0.87 0.77
Water uptake weighted (2)
Whole rootzone 1.79 1.35 1 .O3 0.87 0.77 0.70
(1) Use for conventional irrigation management.
(2) Use for high frequency irrigation management or where matric potential development between irrigations is insignificant.
Table 2: Yields of crops in successive rotation
I
C r o p y e a r
sugar sugar
Treatment Wheat/l982 Beets/l983 Cantaloupes/l983 Wwheatll984 BeetSA985 Cantaloupes/l985
1 ) 4 ) 3 )
2 )
3 ) 5 )
I I
C 3.60 (0.06) ' l ' 4.3 (0.1) 392 (1 2) 3.51 (0.09) 4.1 (0.1) 115 (5)
3.60 4.3 (0.2) 384 (10) 3.46 (0.10) 4.1 (0.1) . 142 ( 8 )
CA 3.71 (0.06) 4.1 (0.1) 355 (1 4) 3.55 (0.09) 3.9 (0.1) 139 (12) 1) C = Colorado River water used solely for irrigation; Alamo River water used in relatively smaller (Ca) and
larger (CA) amounts, after seedling establishments with Colorado River water for wheat and sugar beets.
Cantaloups only irrigated with Colorado River water.
2) Tons grain per acre 3) Tons of sugar per acre 4) Lbs. of seed per acre
Commercial yield in numbers of cartons per plot;
6) '-Value within ( ) is standard error of mean; six replicates plot size = 750 X 38 feet = 0.6543 acres
.
Table 3: Yields of crops in block rotation
Crop year
Treatment Cotton/l982 Cotton/l983 Wheat11 984 A l f a I f a i l 9 %
1 ) 2 ) 4 ) 3 )
C 2.62 (0.07) 2.06 (0.10) 3.43 (0.06) 7.8 (0.4)
CA 2.65 (0.06) 2.00 (0.06) 3.43 (0.06) 7.0 (0.5)
A 2.76 (0.04) 1.32 (0.05) 3.41 (0.05) 7.4 (0.3)
1) C = Colorado River water used solely for irrigation; A = Alamo River used solely for irrigation; CA = Alamo River water used for irrigation after seedling
establishment with Colorado River water for cotton. Wheat and alfalfa irrigated only with Colorado River water
2) Commercial yield of lint, bales per acre 3) Tons of grain per acre
4) Tons of dry hay per acre
5) Value within ( ) is standard error of mean; six replicates
options
O
ü
5
S
O O 2
- S
S
O
c o m a
C U C U C U
c o c o w
e n - Y V W
m - o
c 3
9 8 %
a m * od-CD
n t - 0
N N O
n - &
N o 0
n d - o
O
- 5
S
ò
S
O
' 8 %
S
E S
r- r - a
7
D O O
.- C
- E
Table Estimated evapotranspiration and water lost as deep percolation (inches 1
Accumulated (5)
Crop
v
LFet iw dw i w e t dw
wheat S. beet
melons wheat S. beet melons
cotton cotton wheat alfalfa
Successive crop rotation
Block rotation
Evapotranspiration estimated from pan evaporation and crop factors at Brawley, California Total amount of water applied for irrigation
Estimate of deep-percolation ,drainage water, i.e., Vi.\;
-
(4) Estimate of leaching fraction, i.e., Vd, 'Vi, Accumulated over entire experimental period
options méditerranéennes
Figure l 8: between average rootzone salinity (saturation extract basis), electrical conductivity of irrigation water, and leaching fraction to use
for conditions of conventional irrigation management
o r .
I r l lc
O 4 6 . 8 10 12
Elixfrical Conductivity 01 Irrigation Wafer, dS/m
Figure 2: Salt tolerance of grain crops (after 1977)
5 15 25 . 30 35
Millimhos/Cm
Figure 3: Threshold values of sodium adsorption ratio of topsoil and electrical conductivity of infiltrating water for maintenance of permeability
Areo of unlikely permeability hazard