Effect of Chemical Reclamation
on the Physiological and Chemical Response of Rice Grown in Varying Salinity and Sodicity Conditions
Ayesha Abdul Qadir1, Ghulam Murtaza1*, M Zia-ur-Rehman1 and Ejaz Ahmad Waraich2
1Institute
of Soil and Environmental Sciences, University of Agriculture,
Faisalabad-38040, Pakistan
2Department
of Agronomy, University of Agriculture Faisalabad, Pakistan
*For
correspondence: gmurtazauaf@gmail.com
Received 01 March 2021; Accepted 17 April 2021; Published 10 June 2021
Abstract
Salinity and sodicity are the
major abiotic constraints that prevail in arid and semi-arid regions. Proper
management is required for productive use of this land. Reclamation of sodic
and saline-sodic soils is highly site-specific that describes the diverse
response of different soils to different amendments. These reclamation
practices also alter the plant's physiological and ionic characteristics. This
experiment aimed to better understand the physiological and ionic responses of
rice crop at different salinity/sodicity levels. A lysimeter experiment was set
forth with soil having ECe (dS m-1):SAR (mmol L-1)1/2 levels as 4:20, 8:40, 12:60 and 16:80 and all the levels were treated with organic
(farm manure at 25 Mg ha-1) and inorganic (gypsum at 100% soil gypsum requirement (SGR) and sulphuric acid equivalent to 100% SGR) amendments keeping no ammendment as control.
Results revealed that the maximum relative increase in physiological attributes
(photosynthetic rate, transpiration rate,
stomatal conductance and total chlorophyll contents), ionic contents (nitrogen, potassium and K:Na
ratio) and growth of rice were recorded with sulphuric acid application
followed by gypsum. On an average 25%, 31% and 45% increase in biological
yield, plant height and paddy yield, respectively was observed with sulphuric
acid application over control. It is concluded that sulphuric acid and
gypsum both were the best amendments for reclamation of soil having a low level
of salinity/sodicity whereas, at higher salinity/sodicity levels, only
sulphuric acid seemed better for improved rice production. © 2021 Friends Science Publishers
Keywords: Rice; Gas exchange attributes;
Salinity; Sodicity; Amendments; Reclamation
Introduction
The excess of soluble salts in
agricultural land leads to soil salinity and the conditions become more severe
when sodicity (a high amount of exchangeable sodium (Na+)) prevails,
which not only disturbs the nutrient dynamics but also degrade the soil
structure. Soil salinity and sodicity are two of the world's most important
soil issues, especially in arid and semi-arid regions. Around the globe, above
8 × 108 ha of land is salt degraded either by salinity (3.4 × 108
ha) or sodicity (5.6 × 108 ha) (Shahid
et al. 2018). Salt
degraded area of Asia (194.7 × 106 ha of
saline and 121.9 × 106 ha of sodic) accounts for about 33.9% of the
world’s salt-affected land (Shahid et al. 2018). According to the
estimate of Qadir et al. (2014), negative impacts of salt-affected
irrigated land on crop production could cost the global economy about US$ 27.3
billion annually. In Pakistan, 10 × 106 ha area is currently
affected due to salinity and sodicity and is growing rapidly (Shahid et al. 2018).
Mostly the
salinity and sodicity exist together in soil which means the stress of both
soluble salts and exchangeable Na+ in a medium. Salinity combined
with sodicity is more harmful to plant growth than salinity alone (Abbas et al. 2021). These soils have
less organic matter, a disturbed soil structure, and a lower water holding capability.
Disorganized aggregate formation in these degraded soils affects soil water,
nutrients, and plant development (Nan et al. 2016;
Abbas et al. 2021). The deleterious effects of soil salinity/
sodicity are dependent upon the type and period of salt-affected soil.
Moreover, plant species and their genetic makeup also play a remarkable role (Ata-Ul-Karim et al. 2016; Liu et al. 2020;
Riaz et al. 2020).
Soil salinity
and/or sodicity induce ion toxicity and osmotic stress, and crust formation
affects plant by delaying germination (Ata-Ul-Karim
et al. 2016). Plant growth mechanisms such as photosynthesis,
stomatal conductance, nutrient balance and metabolic functions are all affected
by salinity and sodicity (Nam et al. 2018; Zahra et al. 2018).
The high concentration of NaHCO3/ Na2CO3 under
sodic conditions results in increased pH (> 8.5) that negatively influences
nutrient uptake in plants (Liu et al. 2020). The imbalance of nutrients
(excess of Na+) in plants deteriorates the normal growth process and
ultimately leads to abnormal cell functioning and plant death (Quintero et
al. 2007).
Among the
monocot crops, rice (Oryza sativa L.) is considered salt sensitive
whereas, its tolerance level varies with genotypes because of additive gene
effects (Abbas et al. 2013; Hussain et
al. 2018; Sardar et al. 2018). In the world, 7.55 × 108 t rice has been produced in the year 2018–19 from the total harvested
area of 1.62 × 108 ha with a 4.64 t ha-1 yield. Asia is the biggest rice
producer and consumer and accounts for 92% of the world’s rice production. In
the year 2019, 11.11 × 106
t rice was produced from 3.03 × 106 ha in Pakistan (FAO 2020). Qadir et al. (2014) reported 36–69%
grain yield losses in rice crop due to salinity and sodicity in comparison with
their counterpart normal soils in Pakistan.
Adopting
appropriate diagnosis, reclamation, and land-water management approaches can
help to restore and cultivate these problematic soils and play a significant
role in efficient soil and water conservation. For many decades, chemical
amendments have been used for the reclamation of salt-affected soils (Kheir et al. 2018; Singh et al. 2018;
Zhou et al. 2019). The most commonly used inorganic amendments
include gypsum (Rasouli et al. 2013;
Gonçalo et al. 2020) and sulphuric acid (Mahmoodabadi et al. 2013; Kheir et al. 2018). Organic amendments, such as farm
manure can also be used for the reclamation of salt-affected soils (Ahamed et al. 2019; Leogrande and Vitti 2019).
Amelioration of
sodic and saline-sodic soils is highly site-specific and illustrates how
different soils react to different amendments. Many scientists have noted the
effectiveness of one amendment over another in the context of a single
environment (Kheir et al. 2018; Day et al.
2019). Despite this, the comparison of different responses
of organic and inorganic amendments towards different soil salinity/sodicity
situations requires more investigation in a broad spectrum. According to our
understanding, no comprehensive study was conducted to evaluate crop ionic and physiological activity
changes during the reclamation of sodic and saline-sodic soils using various
organic and inorganic amendments. Therefore, this experiment was executed to
understand the physiological and ionic responses of rice
crop at specific salinity/sodicity levels under the application of different
organic and inorganic amendments. Additionally, screening of appropriate
amendments for the amelioration of soils with different ECe:SAR levels for growing rice crop was
also done.
Materials and Methods
Collection of soils and amendments
Soils used in this experiment were
collected from the naturally degraded and uncultivated
area, Village No. 132/GB (73° 0653, 31° 1903), located near Dijkot district Faisalabad, Pakistan. Bulk of topsoil (0–20 cm) was collected from 2 different points of
barren land. The collected
soil samples were ground, mixed thoroughly,
sieved through a 2 mm stainless steel sieve and prepared
for physicochemical analysis (ECe, pHs, soluble cations and anions) following the procedure described by US Salinity
Lab. Staff (1954). These
soils have variable ECe and SAR (normal and saline-sodic soil) but
have the same textural class (sandy clay loam). The normal soil had ECe= 4.01 dS
m-1, SAR= 8.17 (mmol
L-1)1/2, pHs= 7.44, CaCO3= 4.80%, organic matter= 0.43% and CEC= 9.8 cmolc kg-1. The saline-sodic soil had ECe= 23.5, dS
m-1, SAR= 87.5 (mmol
L-1)1/2, pHs= 8.1. Amendments, i.e., Farm manure (FM) was collected from the dairy
farm of the University of Agriculture, Faisalabad. The
basic characteristics of FM were: EC1:10 = 4.75 dS m-1,
pH of 7.2, total carbon (dry weight basis) = 42%, a total nitrogen (dry weight
basis) = 1.75%, Na+ = 1.28%, K+ = 2.45%. The FM was
air-dried and ground to a fine powder before application. Gypsum (80% pure) was
purchased from a local fertilizer supplier and commercial grade sulphuric acid
(98%) was procured from a local scientific store.
The experiment was carried out in lysimeters using soils with varying salinity/sodicity at wire-house of Institute of Soil and Environmental Sciences, University of Agriculture, Faisalabad, using rice as a
test crop. The metrological conditions of experimental
region during this crop season were ranged as
temperature min 20 and max 31°C, relative humidity 51–62%, maximum rainfall 48 mm and sunshine 6–7 h.
Soils with
varying salinity/ sodicity are described as ECe (dS m-1):SAR (mmol L-1)1/2
levels. Different ECe:SAR levels 4:20, 8:40, 12:60 and 16:80 were
developed by mixing different proportions of normal and
saline-sodic soil. Normal and saline-sodic soils were mixed for each level separately at different proportions
keeping in view their original ECe and SAR value (Table 1).
Polyvinyl chloride lysimeters (internal diameter 26 cm and 64 cm long) were filled
with 42 kg soil after developing designed ECe:SAR
levels of soil. Four lysimeters
in triplicate sets of each ECe:SAR level were maintained. Amendments
including gypsum (G) at 100% soil gypsum requirement (SGR), sulphuric acid (SA) equivalent to 100% SGR and farm
manure (FM) at 25 Mg ha-1 were applied at each level of ECe:SAR and
one control (without addition of any amendment) were kept along. There were 16 treatments and 48 experimental units in total.
Seeds of rice cultivar ‘Super Basmati’ were sown in normal soil and after 35 days, seedlings were
transplanted in soil-filled lysimeters maintaining four plants per lysimeter.
The recommended dose of N:P:K (55:45:32.5 mg kg-1) nutrients
(using urea, diammonium phosphate and sulphate of potash) was applied.
The full dose of P, K and 1/3rd of the recommended dose of N was
applied at the time of transplanting and the remaining N was applied in two
equal splits at tillering and reproductive stages. Throughout the growth period
of crop, canal water having EC 0.25 dS m-1, total soluble salts 2.5 mg L-1, SAR 1.38 (mmol L-1)1/2 and RSC Nil, was used for irrigation as per crop requirement. After 40 days of transplanting rice seedlings, gas exchange attributes, i.e.,
photosynthetic rate, transpiration rate and stomatal conductance were recorded
using a portable narrow chambered infrared gas analyzer (IRGA, LCA-4,
Analytical Development Company, Hoddesdon, England). Leaf total chlorophyll
content index of fully expanded leaves of 40 days old plants were determined via SPAD-502 meter (Minolta, Osaka,
Japan). Average SPAD readings were recorded from three measurements following Saqib et al. (2012). At
maturity, the crop was harvested and different plant growth parameters (plant
height, biological yield and paddy yield) were recorded. Plant samples were safely set aside for
ionic analysis. After harvest, soil
samples were collected from lysimeters for analysis.
Plant digestion and nutrient analysis
Harvested plant samples were washed and set in paper bags separately. These bags were placed in a drying
oven at 70℃ and dried till
the constant weight was achieved. After grinding these plant samples (straw and paddy) in Wiley mill fitted with stainless steel blades, were digested. Di-acid mixture (HNO3:HClO4 2:1 v/v) was used for
this purpose. After digestion, the filtrate
was stored in air-tight bottles. Total N in straw and paddy was determined by micro-Kjeldahl method (Isaac and Johnson 1976). Total P of plant samples was measured on a
UV-visible spectrophotometer (Thermo Electron, Waltham, U.S.A.) after standardizing the instrument with KH2PO4
solutions of known concentration. Total Na and K
were analyzed by Jenway PFP-7 flame photometer using standard curve drawn by
running the solutions of known concentration (prepared using reagent grade NaCl and KCl) on the instrument.
Soil analysis
The
post-rice
harvest soil samples were
collected from lysimeters by using stainless steel sampling tube. Collected
samples were air-dried, ground to pass through a 2 mm sieve and stored in
plastic bags. These samples were analysed for pHs, ECe and soluble cations following
the methods described by the US Salinity Lab. Staff (1954).
Statistical analysis
Experiment was laid out in a factorial completely randomized design
(Factor 1: ECe:SAR levels and
Factor 2: Amendments) with three replications. The data were presented as mean values and the standard errors were
calculated using Microsoft Excel software. The
statistical analyses of data were done using Statistix v. 8.1
computer software. Analysis of variance (two-way ANOVA)
and subsequent pairwise comparison was done with
Tukey’s HSD test at 5% probability. Radar diagrams
were drawn using Origin software (v. 2019,
U.S.A.) by putting relative values of
plant physiological data.
Results
Physiological changes in response to applied amendments at various ECe:SAR levels
Rice physiological parameters
such as photosynthetic rate (A), transpiration rate (E), stomatal
conductance (gs) and total chlorophyll content (SPAD) were significantly
influenced by the ECe:SAR
levels and the type of amendment used, as well as their interaction. The maximum relative increase in SPAD, A, E and gs was observed with SA at all ECe:SAR
levels except ECe:SAR level 12:60 (Fig. 1). All the
recorded physiological data indicated that the increase in ECe:SAR levels results in gradual or sharp
decrease in SPAD, A, E and gs values. The gradual decrease
was observed in SPAD and A whereas E and gs depicted
a sharp decrease at ECe:SAR
level 8:40 and then decrease gradually with increasing ECe:SAR
levels (Fig. 1e).
Growth variations in response to applied amendments at various ECe:SAR levels
As shown in Fig. 2, the
biological yield, plant height and paddy yield were significantly affected with
increasing ECe:SAR
levels and type of applied amendment and their interaction. Sulphuric acid
depicted maximum values for biological yield, plant height and paddy yield
whereas the amendments follow the following sequence in increasing rice growth;
SA > G > FM > C. The maximum increase in biological yield (37.68%
relative to control) was observed at ECe:SAR
level 4:20 with SA. Considering plant height, SA remained best amendment at all
ECe:SAR levels
with the maximum relative increase of 43.76% at ECe:SAR
level 4:20 followed by 40.96% at ECe:SAR
level 16:80 with respect to control. The paddy yield varies between 0.97 to
3.86 g plant-1 with maximum value at ECe:SAR level 4:20 and minimum value at
level 16:80.
Ionic variations in response to applied amendments at various ECe:SAR levels
Nitrogen: Nitrogen
(N) concentration in straw and paddy was significantly influenced with ECe:SAR levels, type of
amendment and their interaction. In straw, N concentration varied between 0.40
and 0.65%, with maximum concentration at ECe:SAR
level 12:60 and minimum at ECe:SAR level
4:20 (Table 2). A promising increase in N was observed with SA (24 to 36% with
respect to respective controls) at all ECe:SAR levels. In case of paddy, the maximum
value (1.11%) was recorded with G at ECe:SAR
level 12:60 and the minimum (0.72%) was observed with control at ECe:SAR level 16:80 (Table 2).
Phosphorus: The straw phosphorus (P)
concentration shows a variable trend with respect to both ECe:SAR level and amendments (Table 2).
However, the studied factors and their interaction have a significant effect.
The P concentration in rice straw was ranged from 0.10 to 0.03%. The maximum
relative increase in straw P concentration was observed with FM at ECe:SAR level 8:40 and
12:60. Paddy P concentration was significantly varied with different ECe:SAR levels and amendments. The maximum P
concentration in paddy was observed with SA at ECe:SAR level 4:20 whereas, G showed
better results at levels 8:40 and 12:60. At ECe:SAR
level 16:80, FM performed best regarding paddy P concentration.
Fig. 1: Radar charts representing variation in physiological
parameters of rice due to ECe: SAR level a)
4:20, b) 8:40, c) 12:60 and d) 16:80. The status of
physiological parameters with FM (red), G (green) and SA (blue) is shown
relative to the control (C= black). e) Line chart representing the
relative effect of ECe: SAR levels on
physiological parameters. * =value is presenting as divisor of 4. C= Control;
FM= Farm manure at 25 Mg ha-1; G= Gypsum at 100% SGR; SA= Sulphuric acid equivalent to 100% SGR. SPAD= Total
chlorophyll contents, A=Photosynthetic rate, gs=
Stomatal conductance and E= Transpiration rate
Common alphabets above points at an
antenna represents non-significant difference at P ≤ 0.05
Fig. 2:
Effect of ECe: SAR levels and amendments
on growth parameters of rice (a) biological yield (g plant-1),
(b) plant height (cm) and (c) paddy yield (g plant-1).
C= Control;
FM= Farm manure at 25 Mg ha-1; G= Gypsum at 100% SGR; SA= Sulphuric acid equivalent to 100% SGR. Bars denote standard
error (n=3). Common alphabets above bars represent
non-significant difference at P ≤ 0.05
K:Na ratio: There was a significant variation
in straw and paddy potassium:sodium ratio (K:Na ratio) due to ECe:SAR levels, applied amendments and their
interaction (Table 2). In straw, K:Na ratio varied between 0.42 and 3.58
whereas in paddy, values for K:Na ratio lies between 0.72 and 6.23. The highest
values for straw and paddy K:Na ratio was observed with SA treatment whereas
these values decreased as ECe:SAR
level increased.
Variation in post-harvest soil chemical properties due to applied amendments at
various ECe:SAR
levels
Table 1: Characteristics of soils used for rice cultivation after
developing required ECe: SAR levels prior
to the experiment
Desired ECe:SAR |
Achieved ECe:SAR |
pHs |
4:20 |
04.5: 20.42 |
7.82 |
8:40 |
07.9: 38.28 |
8.51 |
12:60 |
12.4: 60.38 |
8.7 |
16:80 |
16.0: 80.23 |
8.81 |
ECe (dS m-1) and SAR (mmol
L-1)1/2
Table 2:
Effect of ECe: SAR levels and amendments
on rice straw and paddy ions content
ECe:
SAR level |
N (%) |
P (%) |
K (%) |
Na (%) |
K:Na ratio |
||||||
Amendment |
Straw |
Paddy |
Straw |
Paddy |
Straw |
Paddy |
Straw |
Paddy |
Straw |
Paddy |
|
4:20 |
C |
0.40 g |
0.81 h |
0.05 fg |
0.21 b-e |
0.76 ab |
0.25 abc |
0.327 i |
0.050 de |
2.34 c |
5.11 bc |
FM |
0.45 e |
0.85 gh |
0.06 e |
0.24 ab |
0.81 a |
0.27 ab |
0.290 ij |
0.059 cde |
2.80 b |
4.49 cd |
|
G |
0.50 d |
0.92 ef |
0.08 c |
0.24ab |
0.85 a |
0.28 a |
0.307 i |
0.049 de |
2.77 b |
5.68 ab |
|
SA |
0.52 cd |
0.96 de |
0.10 b |
0.26 a |
0.86 a |
0.29 a |
0.240 j |
0.048 e |
3.58 a |
6.23 a |
|
8:40 |
C |
0.45 e |
0.83 gh |
0.06 e |
0.19 def |
0.51 ef |
0.20 de |
0.477 g |
0.079 c |
1.07 ef |
2.51 g |
FM |
0.50 d |
0.88 fg |
0.10 a |
0.22 bcd |
0.62 cd |
0.22 cde |
0.443 gh |
0.070 cde |
1.40 de |
3.12 efg |
|
G |
0.54 c |
1.00 d |
0.08 c |
0.23 abc |
0.64 cd |
0.23 bcd |
0.403 h |
0.061 cde |
1.61 d |
3.69 de |
|
SA |
0.61 b |
1.07 ab |
0.07 d |
0.20 cde |
0.68 bc |
0.23 bcd |
0.413 h |
0.066 cde |
1.65 d |
3.54 ef |
|
12:60 |
C |
0.51 d |
0.93 ef |
0.05 gh |
0.19 c-f |
0.42 fg |
0.18 ef |
0.667 bc |
0.117 b |
0.64 ghi |
1.57 h |
FM |
0.61 b |
1.01 cd |
0.10 b |
0.14 g |
0.55 de |
0.20 de |
0.623 cde |
0.080 c |
0.88 fgh |
2.50 g |
|
G |
0.62 ab |
1.11 a |
0.06 de |
0.20 c-f |
0.55 de |
0.21 cde |
0.583 ef |
0.071 cd |
0.95 fg |
2.99 efg |
|
SA |
0.65 a |
1.09 ab |
0.05 f |
0.16 fg |
0.58 cde |
0.22 cde |
0.553 f |
0.074 c |
1.05 ef |
3.05 efg |
|
16:80 |
C |
0.41 fg |
0.72 i |
0.03 j |
0.20 cde |
0.33 g |
0.15 f |
0.780 a |
0.210 a |
0.42 i |
0.72 i |
FM |
0.43 ef |
0.85 gh |
0.04 i |
0.22 bcd |
0.41 fg |
0.18 ef |
0.713 b |
0.120 b |
0.57 hi |
1.53 hi |
|
G |
0.50 d |
0.99 d |
0.04 i |
0.17 efg |
0.48 ef |
0.20 de |
0.643 cd |
0.079 c |
0.75 f-i |
2.46 g |
|
SA |
0.51 cd |
1.06 bc |
0.04 hi |
0.14 g |
0.51 ef |
0.20 de |
0.590 def |
0.076 c |
0.87 fgh |
2.71 fg |
Common alphabets in a column followed by values represents non-significant difference
at P ≤ 0.05. C= Control; FM= Farm manure at 25 Mg ha-1; G=
Gypsum at 100% SGR; SA= Sulphuric acid equivalent to
100% SGR; N= Nitrogen; P=Phosphorus; K= Potassium; Na= Sodium.
Table 3: Effect of ECe:
SAR levels and amendments on chemical characteristics of soil
ECe: SAR level |
Amendments |
ECe |
RP |
SAR |
RP |
pHs |
4:20 (4.5: 20.4)* |
C |
3.20 gh |
-28.89 |
17.17 h |
-15.85 |
7.58 cd |
FM |
2.44 hi |
-45.85 |
13.83 i |
-32.21 |
7.62 c |
|
G |
1.34 ij |
-70.23 |
12.98 i |
-36.36 |
7.55 cde |
|
SA |
1.25 j |
-72.33 |
12.06 i |
-40.90 |
7.29 fg |
|
8:40 (07.9: 38.28)* |
C |
6.88 e |
-12.95 |
35.34 e |
-7.68 |
8.30 b |
FM |
4.16 fg |
-47.31 |
26.76 f |
-30.09 |
7.37 efg |
|
G |
4.37 f |
-44.74 |
20.43 g |
-46.64 |
7.38 d-g |
|
SA |
3.88 fg |
-50.89 |
20.92 g |
-45.34 |
7.33 fg |
|
12:60 (12.4: 60.38)* |
C |
10.69 b |
-13.76 |
52.32 b |
-13.35 |
8.67 a |
FM |
7.81 de |
-36.99 |
40.21 cd |
-33.41 |
8.29 b |
|
G |
7.30 de |
-41.10 |
28.56 f |
-52.69 |
7.63 c |
|
SA |
6.77 e |
-45.40 |
26.47 f |
-56.17 |
7.45 c-f |
|
16:80 (16.0: 80.23)* |
C |
12.78 a |
-20.13 |
70.24 a |
-12.45 |
8.62 a |
FM |
9.03 c |
-43.58 |
50.77 b |
-36.72 |
8.36 b |
|
G |
8.29 cd |
-48.19 |
42.01 c |
-47.63 |
7.36 efg |
|
SA |
7.06 e |
-55.90 |
38.28 d |
-52.29 |
7.20 g |
*achieved values; Unit of ECe
and SAR are dS m-1 and (mmol L-1)1/2,
respectively. Common alphabets in a column followed by values represents
non-significant difference at P
≤ 0.05. RP= relative percentage. (-) sign indicates relative decrease. C=
Control; FM= Farm manure at 25 Mg ha-1; G= Gypsum at 100% SGR; SA= Sulphuric acid equivalent to 100% SGR
The
present experiment revealed the beneficial effect of applied amendments, i.e., SA, G and FM in
decreasing ECe, SAR and pHs, of post-rice harvest soil (Table 3). Application of amendments
directly or indirectly increased Ca2+ and Mg2+ in soil solution that possibly replace the Na+ present on
exchange sites of soil colloids and reduces the SAR of soil. This replaced Na+
came into the soil solution and was effectively removed from the rooting zone
along with other soluble salts with the application of good quality water,
which ultimately reduced the ECe of soil (Gharaibeh et al. 2010; Gonçalo et
al. 2020). The
role of SA was noticeable in decreasing ECe, SAR and pHs of soil (Table 3). Previously considerable decrease
in ECe, SAR and pHs of soil with SA
have been reported by Mahmoodabadi
et al. (2013) and Ahmad
et al. (2013). The promising effect of SA in reducing SAR individually
or in combination with other organic and inorganic amendments was also observed by Mahmoodabadi
et al. (2013) and indicates the supremacy of SA over
G in ameliorating sodicity. This might be due to the faster dissolution of lime with acid than the
gypsum dissolution (Amezketa et al. 2005).
In the current experiment, improvement
in physiological attributes (SPAD, A, gs and
E) with SA were promising compared with other applied amendments but in some treatments, G also performed good (Fig. 1). Cha-Um et al. (2011)
reported a significant positive effect of G and
FM on SPAD, A, gs and
E of rice plant grown in salt-affected soil. The reaction of SA with soil
lime, increase both soluble Ca2+ and SO42-
(Mace et al. 1999) that play the key role in nullifying salt stress and
improving physiological and growth characteristics in various plants (Helmy et
al. 2013; Akladious and
Mohamed 2018; Hussain et
al. 2019; Riffat et al. 2020). The alleviation in rice SPAD, A, gs and
E also attributed to improved
nutrients uptake, which plays a considerable role in the photosynthetic
process, stomatal movement, osmoregulation and enzyme activation (Hasanuzzaman et al. 2018).
Application of amendments
significantly increased N, P and K contents at all ECe:SAR
levels in rice straw and paddy (Table 2).
Previous research has also shown that organic and inorganic amendments increase nutrient content (Helmy et al. 2013; Singh et
al. 2018; Sardar et al. 2021). Overall,
the highest straw and paddy N and K contents were observed with
SA. However, the response of P
was variable. Shaban et al. (2013) found the highest N, P and K content
with SA compared to G and elemental sulphur in sandy loam soil having
ECe 14.8 dS m-1 and SAR 22.9. Such improvements may be
due to the lowering of pH, ECe and SAR of the treated soil through
amendment addition and improving utilization of
essential plant nutrients (Mazhar et al. 2011;
Shaban et al. 2013). The synergistic
effect of SA on N, P and K availability and uptake was
also reported by Helmy et al. (2013). In contrast, it was observed that
rice Na+ contents significantly decreased with the application of
SA. As applied amendments play a significant role in saline-sodic soil
reclamation and removal of excessive Na+ from root zone and thus
reduce the entry of Na+ in plants and consequently increase K:Na
ratio of a plant (Jedrum et al. 2014).
Plant height, biological yield and paddy yield (Fig. 2) varied significantly at different ECe:SAR levels as well as with different
amendments. Similar to our results,
many researchers have demonstrated that rice yield decreases with an increase
in salt stress (Hussain et al. 2012, 2013; Hakim et al. 2014; Huang et al. 2017). At
higher ECe:SAR
levels, diminished rice growth attributed to
increased salinity and sodicity level than rice threshold limit, that causes osmotic effect and disturb plant ionic
status. The reported threshold salinity
level for rice ranged 1.9–3.0 dS m-1 (Grieve et
al. 2012) and may decrease the yield greater than 50% at an ECe
of 6.65 dS m-1 (Cha-Um et
al. 2011) whereas it could grow unaffectedly up to exchangeable
sodium percentage level 40 (Abrol and Bhumbla 1979).
Hakim et al. (2014) explained the reduction of grain yield
under salt stress as excess salts alter the
metabolic activities of the cell wall,
limiting its elasticity. As a result, the cell wall becomes rigid and reduced the
turgor pressure efficiency in cell enlargement.
Rice plant height,
paddy yield and biological yield significantly increased with the
application of SA, G and FM, whereas, the growth with SA
amendment was considerably high (Fig. 2). The superiority
of SA might because of its effect on decreasing
soil pH, improving soil aggregation and
enhancing the availability of certain
plant nutrients (Niazi et al. 2001; Kheir et al. 2018). Helmy et al. (2013)
credited the improvement in growth parameters to direct and indirect source of
Ca2+, that is required for a variety of plant functions, among which appropriate cell division and elongation, enzyme activity and
metabolism are primary. Similar results were also
reported by Mazhar et al. (2011) and Saqib et al. (2019).
Conclusion
This
research documented two main outcomes. First, among
the amendments examined, at lower ECe:SAR
levels (4:20, 8:40 and
12:60), the responses of sulphuric acid and gypsum were
identical, but at higher level (16:80)
sulphuric acid was more effective. Secondly, the disturbance in rice photosynthetic
rate, stomatal conductance, transpiration rate and
total chlorophyll contents due to salinity/sodicity stress
were significantly overcomed with sulphuric acid treatment. Moreover, the
improvement in N and K contents, K:Na ratio and biological and paddy yield were
significantly consistent with the effectiveness of soil salinity/sodicity
ameliorating treatment.
Acknowledgements
This research work was supported
by National Research Program for Universities- Higher Education Commission
(HEC), Islamabad, Pakistan (NRPU # 4926) and HEC Indigenous
scholarship program.
Author
Contributions
AAQ and GM conceptualized, AAQ
investigate, statistical analyzed the data, write and prepare original draft,
ZR and EAW review and edit the draft.
Conflict of Interest
Authors declare no
conflict of interest.
Data Availability
The data will be made
available on reasonable request to the corresponding author.
Ethics Approval
Not applicable.
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