The Scientific World Journal
Volume 2015 (2015), Article ID 906094, 14 pages
http://dx.doi.org/10.1155/2015/906094

Research Article

Improving Lowland Rice (O. sativa L. cv. MR219) Plant Growth Variables, Nutrients Uptake, and Nutrients Recovery Using Crude Humic Substances

Perumal Palanivell,¹ Osumanu Haruna Ahmed,1,2,3 Nik Muhamad Ab Majid,³ Mohamadu Boyie Jalloh,⁴ and Kasim Susilawati¹

¹Department of Crop Science, Faculty of Agriculture and Food Sciences, Universiti Putra Malaysia Bintulu Sarawak Campus, 97008 Bintulu, Sarawak, Malaysia
²Agriculture and Environment, Borneo Eco-Science Research Center, Faculty of Agriculture and Food Sciences, Universiti Putra Malaysia Bintulu Sarawak Campus, 97008 Bintulu, Sarawak, Malaysia
³Institute of Tropical Forestry and Forest Products (INTROP), Universiti Putra Malaysia, 43400 Serdang, Selangor, Malaysia
⁴Faculty of Sustainable Agriculture, Universiti Malaysia Sabah Kampus Sandakan, Locked Bag No. 3, 90509 Sandakan, Sabah, Malaysia

Received 6 February 2015; Accepted 3 April 2015

Academic Editor: Antonio Ferrante

Copyright © 2015 Perumal Palanivell et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

Abstract.

High cation exchange capacity and organic matter content of crude humic substances from compost could be exploited to reduce ammonia loss from urea and to as well improve rice growth and soil chemical properties for efficient nutrients utilization in lowland rice cultivation. Close-dynamic air flow system was used to determine the effects of crude humic substances on ammonia volatilization. A pot experiment was conducted to determine the effects of crude humic substances on rice plant growth, nutrients uptake, nutrients recovery, and soil chemical properties using an acid soil mixed with three rates of crude humic substances (20, 40, and 60 g pot⁻¹). Standard procedures were used to evaluate rice plant dry matter production, nutrients uptake, nutrients recovery, and soil chemical properties. Application of crude humic substances increased ammonia volatilization. However, the lowest rate of crude humic substances (20 g pot⁻¹) significantly improved total dry matter, nutrients uptake, nutrients recovery, and soil nutrients availability compared with crude humic substances (40 and 60 g pot⁻¹) and the normal fertilization. Apart from improving growth of rice plants, crude humic substances can be used to ameliorate acid soils in rice cultivation. The findings of this study are being validated in our ongoing field trials.

1. Introduction

Ultisols and Oxisols are the most common agricultural soils in the tropics. Besides being highly weathered, these soils are acidic, very low in cation exchange capacity (CEC), and inherently low in nutrients [1]. The large amounts of oxides and hydroxides of Fe and Al in Ultisols and Oxisols have been associated with the abundance of variable charge colloids, low pH, and low CEC [2, 3]. These oxides and hydroxides commonly fix large amounts of soluble phosphate leading to low concentrations of available Phosphorus (P) in soil solution [4, 5]. Furthermore, in lowland rice fields (waterlogged condition) urea is mostly lost through NH₃ volatilization. Ammonia volatilization is higher in waterlogged condition compared to nonwaterlogged condition [6, 7] and this NH₃ volatilization occurs when urea is hydrolyzed to ammonium carbonate (equation (1)). Subsequently, ammonium carbonate decomposes into CO₂, H₂O, and NH₃ (equations (2) and (3)) [8].

Urea Hydrolysis

Thus the aforementioned problems lead to nutrients unavailability for rice plant growth and development. To overcome the stated problems, farmers apply fertilizers excessively to attain higher yield. However, unbalanced use of N and P fertilizers causes environmental problems such as eutrophication, groundwater pollution, acid rain deposition, soil acidification, and greenhouse gas emissions [9–12].

Utilization of humic substances in acidic soils was reported not only to have reduced Al³⁺ and Fe²⁺ but also to have increased P [13]. Reduction of Al³⁺ and Fe²⁺ ions in soil solution is essential as this prevents P from being precipitated as strengite, vivianite, variscite, and various minerals of the plumbogummite group [14]. Moreover, P fixation in acid soils can be reduced by increasing soil pH as availability of P varies with variation in soil pH. For example, most of P is available for plant uptake at neutral pH [8]. This suggests that the sawdust ash used to extract crude humic substances in this study can be exploited to increase pH of acidic soils because of their basic nature (pH 11). Crude humic substances which are produced from rice straw compost and sawdust ash can also be used to improve soil chemical properties because these organic substances can increase soil pH and organic matter [15]. Additionally, the high CEC of rice straw compost can be exploited to improve CEC of acid soils and to as well retain cations such as , K⁺, Ca²⁺, and Mg²⁺. In addition, good retention of cations including ion, ammonia volatilization from urea, and nutrients leaching could be significantly reduced. Ammonia volatilization from urea as an example can be reduced with application of materials which are high in CEC [16–18]. Humic substances which are high in CEC have been used to control ammonia volatilization in nonwaterlogged condition. In nonwaterlogged conditions, humic acids and fulvic acids from tropical peat, coal, palm oil mill effluent sludge, and crude humins from composts [19–23] have been used to reduce NH₃ loss from urea. In waterlogged soils, Clinoptilolite zeolite has been used to reduce ammonia volatilization [17, 18, 24].

Apart from fewer studies which had been carried out to determine the effects of humic substances on ammonia loss and soil chemical properties of waterlogged soil, isolation (extraction, fractionation, and purification) of humic acids, fulvic acids, and humins is laborious and expensive. Hence, in this present study, rice straw compost was rather mixed with sawdust ash to produce crude humic substances. We hypothesized that the application of crude humic substances which are high in CEC could reduce NH₃ volatilization from urea, increase rice plant growth, nutrients uptake, recovery, and as well improving soil chemical properties in waterlogged condition. Thus, this study was conducted to determine the effects of mixing an acid soil (Typic Paleudults) with crude humic substances at three rates (20, 40, and 60 g pot⁻¹) in waterlogged condition on NH₃ volatilization from urea, rice plant growth, nutrients uptake, and recovery and improve soil chemical properties.

2. Materials and Methods

2.1. Soil Sampling, Preparation, and Characterization

Typic Paleudults (Bekenu Series) soil was sampled at 0 to 25 cm in an uncultivated area of Universiti Putra Malaysia Bintulu Sarawak Campus, Malaysia (latitude 3°12′N and longitude 113°4′E). The soil was air-dried, ground, and sieved to pass to a 5 mm sieve. The soil was analyzed before and after the pot study for pH in distilled water (at ratio of 1 : 2.5 soil : water) using a digital pH meter [25], total carbon using loss-on-ignition method [26], total organic carbon (TOC) and organic matter (OM) content using Walkley-Black method [27], cation exchange capacity (CEC) using the ammonium acetate leaching method [28], total N using Kjeldahl method [29], and available and exchangeable [30]. Exchangeable cations and available P were extracted using the Double Acid Method [31], after which cations were determined using Atomic Absorption Spectrometer (AAnalyst 800, Perkin Elmer Instruments, Norwalk, CT), whereas available P was determined using the Blue Method [32]. Total titratable acidity was determined using acid-base titration method [33]. The selected chemical and physical properties of the soil (Table 1) used in this study are typical of Typic Paleudults (Bekenu series) and they are consistent with those reported by Paramananthan [34] except for CEC, exchangeable calcium, and magnesium.

Table 1: Selected chemical properties of Typic Paleudults (Bekenu Series) soil before incubation and pot study.

Property
Current study
Standard data range* 
(0–36 cm)

4.41
4.6–4.9

Bulk density (g cm⁻³)
1.16
NA

TOC (%)
1.43
0.57–2.51

Total N (%)
0.08
0.04–0.17

Exchangeable (mg kg⁻¹)
21.02
NA

Available (mg kg⁻¹)
7.01
NA

Available P (mg kg⁻¹)
4.85
NA

(Cmol (+) kg⁻¹)

CEC
11.97
3.86–8.46

Exchangeable K⁺
0.10
0.05–0.19

Exchangeable Ca²⁺
0.25
NA

Exchangeable Mg²⁺
0.34
NA

Exchangeable Na⁺
0.22
NA

Exchangeable Fe²⁺
0.19
NA

Exchangeable Cu²⁺
Trace
NA

Exchangeable Zn²⁺
0.01
NA

Exchangeable Mn²⁺
0.02
NA

Total titratable acidity
0.86
NA

Exchangeable H⁺
0.64
NA

Exchangeable Al³⁺
0.22
NA

NA: not available; *Paramanathan [34].

2.2. Rice Straw Compost and Sawdust Ash Production

The compost used in this study is produced from mixture of rice straw (75%) + chicken dung (15%) + molasses (6%) + urea (2%) + rock phosphate (2%) [35]. Sawdust dust was incinerated at 600°C using muffle furnace for 10 hours in an aluminium ware (size 30 cm length × 17 cm width × 8 cm height) until almost white ash is produced.

2.3. Rice Straw Compost and Sawdust Ash Characterization

The rice straw compost and sawdust ash were analyzed for pH in distilled water (at ratio of 1 : 10 compost : water; 1 : 100 ash : water) using a digital pH meter [25], total N using Kjedahl method [29], CEC using the ammonium acetate leaching method [28], organic matter, and total organic carbon content using loss-on ignition method [36]. Total P and cation contents in the rice straw compost and sawdust ash were extracted using the single dry ashing method [28]. Phosphorus in the extract was quantified using the Blue Method [32], whereas cations content were determined using atomic absorption spectrophotometer (AAnalyst 800, Perkin Elmer Instruments, Norwalk, CT). The molarity of sawdust ash (at ratio of 1 : 100 ash : water) was determined using acid-base titration [37] with modification of 180 rpm instead of 150 rpm. Humic acids and crude humins content in rice straw compost were determined using method of Ahmed et al. [38] and Palanivell et al. [35, 39]. Total organic carbon, organic matter content, humic acids, and CEC of the rice straw compost and pH and total calcium content of the sawdust ash were higher as expected (Table 2).

Table 2: Selected chemical properties of rice straw compost and sawdust ash.

Property
Rice straw compost
Sawdust ash

pH
7.58
11.03

CEC (Cmol (+) kg⁻¹)
93.60
nd

Molarity (w : v = 1 : 100) (M)
nd
0.002

(%)

Organic matter
74.00
nd

Total organic carbon
42.92
nd

Humic acids
10.97
nd

Crude humins
87.93
nd

Total N
1.85
nd

Total P
0.75
0.47

Total K
2.42
0.27

Total Ca
1.20
7.63

Total Mg
0.75
1.09

Total Na
0.24
0.04

Total Fe
0.25
3.57

Total Zn (mg kg⁻¹)
164
683

Total Mn (mg kg⁻¹)
223
1833

Total Cu (mg kg⁻¹)
71
213

2.4. Treatments Evaluation for Ammonia Loss from Urea

The ammonia loss incubation study was conducted using close-dynamic air flow system [40, 41]. Treatments were arranged in a Completely Randomized Design (CRD) with three replications. The treatments per 250 g of soil evaluated in 500 mL conical flask were as follows.

(i)C1: soil alone.(ii)C2: soil + complete fertilization.(iii)CHS1: soil + complete fertilization + 20 g rice straw compost + 2 g sawdust ash.(iv)CHS2: soil + complete fertilization + 40 g rice straw compost + 4 g sawdust ash.(v)CHS3: soil + complete fertilization + 60 g rice straw compost + 6 g sawdust ash.

The complete fertilization is equivalent to 1.31 g urea + 1.39 g ERP + 0.88 g MOP + 0.16 g Kieserite + 0.53 g chelated ZnCoBor per experimental unit. The amounts of fertilizers used were scaled down for plant density of 3 rice plants hill⁻¹. This fertilizer rate (151 kg ha⁻¹ N, 97.8 kg ha⁻¹ P₂O₅, 130 kg ha⁻¹ K₂O, and 7.6 kg ha⁻¹ MgO) was based on the recommended fertilizer for rice by Muda Agricultural Development Authority, Malaysia [42], with additional micronutrients (2.3 kg ha⁻¹ B, 4 kg ha⁻¹ Cu, and 4 kg ha⁻¹ Zn) [43]. The amounts of rice straw compost used in this study were deduced from the literature [44–49], where 5, 10, and 15 tons ha⁻¹ equivalent to 20, 40, and 60 g pot⁻¹ were used.

The incubation study was carried out by mixing soil with rice straw compost and sawdust ash for the treatments with crude humic substances alone after which the mixture was moistened to 100% of field capacity and left overnight to equilibrate. Before the fertilizers were applied, the water level in each conical flask was maintained at 3 cm from the soil surface to ensure that the system was waterlogged. The water level was marked on the conical flasks. The water level in the conical flask was maintained throughout incubation period (33 days) by adding distilled water as the deficit of the original water level. The fertilizers were applied on the soil surface, and air was passed through the volatilization system at a rate of 2.5 L min⁻¹ and volatilized ammonia from urea was captured in 75 mL of 2% boric acid solution with bromocresol green and methyl red indicator. The rate of air flow was measured using a Gilmont flow meter (Gilmont Instrument, Great Neck, NY, USA). The boric acid solution was replaced every 24 h and back titrated with 0.05 M HCl to determine ammonia loss from urea. This measurement was continued until the ammonia loss decreased to 1% of the N added in the system [24, 40].

2.5. Germination Media Selection

Before the pot study, germination media selection was done using rice seeds variety of MR219 (commonly used rice seed in Malaysia). This study was carried out using plastic ware measuring 17 cm (length) × 12 cm (width) × 6.5 cm (height) filled with 100 g of germination media and the media were moistened up to 100% of its field capacity. The river sand used in this study was washed with tap water after which it was washed thoroughly with distilled water until the pH of the sand was neutral (pH 7). Ten rice seeds were seeded on each germination medium. The experimental design was Completely Randomized Design (CRD) with 3 replications. The treatments evaluated were as follows.

(i)G1: 100% sand(ii)G2: 5% rice straw compost + 95% sand(iii)G3: 10% rice straw compost + 90% sand(iv)G4: 15% rice straw compost + 85% sand

After 7 days of seeding, germination rate, root elongation, and shoot elongation were measured using a digital vernier caliper whereas relative seed germination, germination index, relative root elongation, and relative shoot elongation of rice seedling were determined as described by Araújo and Monteiro [50]. The ammonia volatilization and germination medium selection studies were conducted in a laboratory at the Research Center of Universiti Putra Malaysia Bintulu Sarawak Campus, Malaysia, which had an average temperature of 29.6°C (range 26.8–31.9°C) and an average relative humidity of 71.0% (range 50.1–85.1%).

2.6. Pot Study

The quantity of the soil used in the pot study was calculated based on the soil’s bulk density. A 1 kg of air-dried soil was filled in a pot measuring 12.5 cm (top diameter) × 10 cm (bottom diameter) × 9 cm (height). Before planting, rice seeds variety of MR219 were germinated in a plastic ware filled with germination medium (100% sand) which was selected from the germination medium selection study. The treatments evaluated in this pot study were the same as those used in the ammonia volatilization study. However, fertilization was done as summarized in Table 3.

Table 3: Fertilization schedule for the pot study.

Days after seeding (DAS)
Urea
ERP
MOP
Kieserite
Zncobor

(g pot⁻¹)

15 DAS
0.55
0.79
0.24
—
—

35 DAS
0.40
—
0.24
0.06
0.53

50 and 70 DAS
0.18
0.30
0.20
0.05
—

The pots were filled with soil only in C1 and C2. For CHS1, CHS2, and CHS3, soil was mixed thoroughly with different rates of crude humic substances (20, 40, and 60 g pot⁻¹) according to the treatments. Crude humic substances were prepared by mixing sawdust ash, rice straw compost, and water thoroughly (at ratio of 1 : 10 : 100) and left for 24 h before mixing with soil. Potting was done 24 h before transplanting. The water level in each pot was maintained at 2 cm from the soil surface. At 7 days after seeding, rice seedlings were transferred into pots (planting density of 3 seedlings per pot which is equivalent to 3 seedlings hill⁻¹) [51]. This pot trial was carried out in a rain shelter at Universiti Putra Malaysia Bintulu Sarawak Campus, Malaysia, and the treatments were arranged in Completely Randomized Design (CRD) with 4 replications. The experimental area has total precipitation of 753 mm, average relative humidity of 85% (range 70–95%), and mean minimum and maximum temperatures of 23.3°C and 32.7°C, respectively, throughout the study period [52].

Plant height, number of tillers, and number of leaves were recorded at harvest (90 days after seeding). The rice plants were harvested and partitioned into aboveground biomass and root before heading stage (end of vegetative stage). This was due to the insufficient amount of soil to support rice plant up to reproduction stage. Besides, it is not economically practical to estimate yield of rice based on pot experiment. The plant parts were oven-dried at 60°C until a constant weight obtained. The oven-dried plant samples were ground using Retsch SM100 comfort cutting mill (Retsch GmbH, Germany) after which they were analyzed for total N [29] and crude silica [53]. The plant samples were digested using the single dry ashing method [28] after which K, Ca, Mg, Cu, Zn, Fe, and Mn contents were determined using atomic absorption spectrophotometer (AAnalyst 800, Perkin Elmer Instruments, Norwalk, CT) whereas P was determined using Molybdenum Blue Method [32]. Nutrient uptake was calculated by multiplying nutrient content with plant dry weight. Rice plant nutrient recovery was calculated using the method of Dobermann [54].

2.7. Statistical Analysis

Analysis of variance (ANOVA) was used to detect significant differences among treatments whereas Tukey’s test was used to compare treatment means using Statistical Analysis System version 9.2 [55].

3. Results and Discussion

Ammonia volatilization was observed for soil with complete fertilization without crude humic substances (C2) and soil with crude humic substances (CHS1, CHS2, and CHS3) on the first day of incubation (Figure 1). Ammonia loss from C2, CHS1, CHS2, and CHS3 lasted for 32 days. Ammonia volatilization decreased at 6, 11, 18, and 24 days of incubation and increased at 7, 12, 19, and 25 days of incubation in all the treatments except for C1. The fluctuation in ammonia volatilization during the incubation study was due to the reaction between urea and soil water to form [24, 56]. As the soil surface rapidly dried due to air velocity in the chamber, NH₃ from urea decreased at 6, 11, 18, and 24 days of incubation. Ammonia loss decreased when soil water was insufficient for the chemical reaction and it increased at 7, 12, 19, and 25 days of incubation upon addition of water. This observation is consistent with that of Bundan et al. [56] and Palanivell et al. [24]. No ammonia volatilization in soil alone (C1) suggests that soil alone did not contribute to ammonia loss. This observation is consistent with findings reported in previous studies [41, 56].

Figure 1: Daily ammonia loss for different treatments (C1: soil alone, C2: soil + complete fertilization, CHS1: soil + complete fertilization + 20 g rice straw compost + 2 g sawdust ash, CHS2: soil + complete fertilization + 40 g rice straw compost + 4 g sawdust ash, and CHS3: soil + complete fertilization + 60 g rice straw compost + 6 g sawdust ash) over 33 days of incubation.

Treatments with crude humic substances (CHS1, CHS2, and CHS3) showed higher NH₃ loss compared to the normal fertilization (C2) (Figure 2). The basic nature of the sawdust ash (pH 11.03) used in this study might have contributed to the NH₃ volatilization in the treatments with crude humic substances (CHS1, CHS2, and CHS3). This is because rapid conversion of ions to NH₃ gas during urea hydrolysis occurs at higher pH [57, 58]. However, in a related study, application of crude humins from composts in nonwaterlogged condition showed no effect on NH₃ volatilization compared with normal fertilization [23].

Figure 2: Total ammonia loss for different treatments (C1: soil alone, C2: soil + complete fertilization, CHS1: soil + complete fertilization + 20 g rice straw compost + 2 g sawdust ash, CHS2: soil + complete fertilization + 40 g rice straw compost + 4 g sawdust ash, and CHS3: soil + complete fertilization + 60 g rice straw compost + 6 g sawdust ash) at 33 days of incubation. Different alphabets indicate significant difference between means using Tukey’s test at . The error bars are the ± standard error of triplicates.

The effects of all the treatments on seed germination rate, relative germination, relative shoot elongation, relative root elongation, and germination index were statistically similar (Figure 3). Application of rice straw compost (G2, G3, and G4) showed no significant effects on seed germination rate and relative germination. However, rice straw compost (G2, G3, and G4) significantly reduced root elongation and shoot elongation compared with sand alone (G1) (Figure 3). Gallardo-Lara and Nogales [59] demonstrated that high N content in compost and compost rate can cause an inhibitory effect on seed germination and growth. Thus, this germination media test shows that the use of rice straw compost as a germination medium for rice seeds is not suitable. This is further supported by the lower germination index (less than 80%) of the rice seeds on G2, G3, and G4 [50]. In a related study, rice straw was transformed into soil-like substrate through aerobic fermentation and bioconversion using fungi and worms before using the product as a planting medium [60]. Hence, sand alone (G1) was used as germination medium for the rice seedlings production in our pot study.

Figure 3: Treatments (G1: 100% sand, G2: 5% rice straw compost + 95% sand, G3: 10% rice straw compost + 80% sand, and G4: 15% rice straw compost + 85% sand) effect on rice seeds germination rate, shoot elongation, root elongation, relative germination, relative shoot elongation, relative root elongation, and germination index of rice seedlings at 7 days after seeding. Different alphabets indicate significant difference between means using Tukey’s test at . The error bars are the ± standard error of triplicates.

CHS1 and CHS2 significantly improved rice plant height, dry matter production, number of leaves, and tillers compared with normal fertilization (C2) (Figure 4). The lowest crude humic substances rate (CHS1) showed the highest dry matter production compared with other treatments. According to Smith and Dilday [61], high nutrients uptake (especially N and silica) increased rice plant growth and dry matter production, and this observation is consistent with the effect of CHS1 as this treatment showed the highest nutrient uptake (N, crude Si, Ca, Mg, Zn, Cu, and Fe) and recovery (N, Mg, Zn, and Cu) compared with other treatments (Figures 5 and 6). The rice plants under the highest crude humic substances rate (CHS3) died (Figures 4, 5, and 6). The high soil pH (pH 7.13) of CHS3 could be the reason for the rice plant death, because the rice plant variety of MR219 grows well within soil pH of 5.5 to 6.5 [42].

Figure 4: Treatments (C1: soil alone, C2: soil + complete fertilization, CHS1: soil + complete fertilization + 20 g rice straw compost + 2 g sawdust ash, CHS2: soil + complete fertilization + 40 g rice straw compost + 4 g sawdust ash, and CHS3: soil + complete fertilization + 60 g rice straw compost + 6 g sawdust ash) effect on plant height, number of leaves, tillers, and dry matter production of rice plant at 90 days after seeding. Different alphabets indicate significant difference between means using Tukey’s test at . The error bars are the ± standard error of quadruplicates.

Figure 5: Treatments (C1: soil alone, C2: soil + complete fertilization, CHS1: soil + complete fertilization + 20 g rice straw compost + 2 g sawdust ash, CHS2: soil + complete fertilization + 40 g rice straw compost + 4 g sawdust ash, and CHS3: soil + complete fertilization + 60 g rice straw compost + 6 g sawdust ash) effect on N, P, K, crude silica, Ca, Mg, Na, Cu, Zn, Mn, and Fe uptake of rice plant at 90 days after seeding. Different alphabets indicate significant difference between means using Tukey’s test at . The error bars are the ± standard error of quadruplicates.

Figure 6: Treatments (C1: soil alone, C2: soil + complete fertilization, CHS1: soil + complete fertilization + 20 g rice straw compost + 2 g sawdust ash, CHS2: soil + complete fertilization + 40 g rice straw compost + 4 g sawdust ash, and CHS3: soil + complete fertilization + 60 g rice straw compost + 6 g sawdust ash) effect on rice plant N, P, K, Mg, Cu, and Zn recovery at 90 days after seeding. Different alphabets indicate significant difference between means using Tukey’s test at . The error bars are the ± standard error of quadruplicates.

The treatments with crude humic substances (CHS1 and CHS2) showed higher nutrients uptake (K, P, crude Si, Ca, Mg, Na, Mn, and Zn) and recovery (P, K, and Mg) (Figures 5 and 6) compared with normal fertilization (C2). The rice plants with higher crude humic substances (CHS2) showed the highest P uptake and recovery compared with other treatments (Figures 5 and 6) whereas the lowest crude humic substances rate (CHS1) showed the highest uptake of N, crude Si, Ca, Mg, Zn, Cu, and Fe and recovery of N, Mg, Zn, and Cu compared with other treatments (Figures 5 and 6). The highest nutrient uptake and recovery in CHS1 was because of the highest dry matter production in CHS1 (Figure 4).

The treatments with the different rates of crude humic substances (CHS1, CHS2, and CHS3) significantly increased soil pH compared with C1 (soil alone) and C2 (normal fertilization) (Figure 7). Soil pH also increased with increasing rate of crude humic substances (CHS1 < CHS2 < CHS3) (Figure 7) due to the high pH and basic cations of the sawdust ash used in this study (Table 2). Soil total titratable acidity and exchangeable H⁺ were significantly lower in the crude humic substances treatments (CHS1, CHS2, and CHS3) compared with soil alone (C1) and normal fertilization (C2) (Figure 7). The high pH and basic cations of the sawdust ash (Table 2) in CHS1, CHS2, and CHS3 might have reduced soil titratable acidity and exchangeable H⁺. Soil alone treatment (C1) showed the highest total titratable acidity and exchangeable Al³⁺ compared with other treatments because some of the P fertilizer (ERP) in C2, CHS1, CHS2, and CHS3 might have reduced exchangeable Al³⁺ and total titratable acidity compared with soil alone (C1) as in acidic soils, hydroxides and oxides of Al³⁺ are precipitated by as variscite and various minerals of the plumbogummite group [14]. Available P in normal fertilization and crude humic substances (CHS1, CHS2, and CHS3) were statistically similar (Figure 7). However, the highest rate of crude humic substances (CHS3) showed higher available P compared with CHS2. The lower available P in CHS2 compared with CHS3 was due to the higher P uptake and recovery by rice plants under CHS2 as those under CHS3 died.

Figure 7: Treatments (C1: soil alone, C2: soil + complete fertilization, CHS1: soil + complete fertilization + 20 g rice straw compost + 2 g sawdust ash, CHS2: soil + complete fertilization + 40 g rice straw compost + 4 g sawdust ash, and CHS3: soil + complete fertilization + 60 g rice straw compost + 6 g sawdust ash) effect on soil pH, total titratable acidity, exchangeable H⁺, exchangeable Al³⁺, and available P content at 90 days after seeding. Different alphabets indicate significant difference between means using Tukey’s test at . The error bars are the ± standard error of quadruplicates.

CHS1, CHS2, and CHS3 increased soil organic matter (OM), total organic carbon (TOC), total carbon (TC), and cation exchange capacity (CEC) compared with soil alone (C1) and normal fertilization (C2) (Figure 8). Higher OM, TOC, TC, and CEC of the crude humic substances applied soil (CHS1, CHS2, and CHS3) were because of the inherent contents of OM, TOC, TC, and higher CEC of rice straw compost (Table 2). The highest rate of crude humic substances (CHS3) showed the highest soil total N compared to other treatments and this was due to no N depletion in soil because the rice plants could not survive. Normal fertilization (C2) and crude humic substances treatments (CHS1, CHS2, and CHS3) showed similar effect on exchangeable and available . The higher NH₃ volatilization regardless of treatment resulted in lower contents of exchangeable and available in soil (Figure 2).

Figure 8: Treatments (C1: soil alone, C2: soil + complete fertilization, CHS1: soil + complete fertilization + 20 g rice straw compost + 2 g sawdust ash, CHS2: soil + complete fertilization + 40 g rice straw compost + 4 g sawdust ash, and CHS3: soil + complete fertilization + 60 g rice straw compost + 6 g sawdust ash) effect on soil total carbon, total organic carbon, organic matter, cation exchange capacity, exchangeable , available , and total nitrogen content at 90 days after seeding. Different alphabets indicate significant difference between means using Tukey’s test at . The error bars are the ± standard error of quadruplicates.

The effects of the different treatments on selected exchangeable cations at 90 days of seeding are shown in Figure 9. The treatment with the highest rate of crude humic substances (CHS3) showed the highest soil exchangeable K⁺, Ca²⁺, Mg²⁺, Na⁺, Zn²⁺, and Mn²⁺ compared with other treatments due to less nutrients depletion in the soil as the rice plants died during this study. CHS1, CHS2, and CHS3 increased exchangeable Ca²⁺ and Zn²⁺ compared to normal fertilization (C2). The treatment with the lowest crude humic substances (CHS1) showed the highest exchangeable Cu²⁺ compared with other treatments because of antagonistic effect of Cu and Zn [62]. Soil exchangeable Fe²⁺ (CHS1 > CHS2 > CHS3) decreased with increasing rate of crude humic substances (CHS1 < CHS2 < CHS3) due to increase in soil pH (Figure 7) [63].

Figure 9: Treatments (C1: soil alone, C2: soil + complete fertilization, CHS1: soil + complete fertilization + 20 g rice straw compost + 2 g sawdust ash, CHS2: soil + complete fertilization + 40 g rice straw compost + 4 g sawdust ash, and CHS3: soil + complete fertilization + 60 g rice straw compost + 6 g sawdust ash) effect on selected soil exchangeable cations (K⁺, Ca²⁺, Mg²⁺, Na⁺, Cu²⁺, Zn²⁺, Fe²⁺, and Mn²⁺) content at 90 days after seeding. Different alphabets indicate significant difference between means using Tukey’s test at . The error bars are the ± standard error of quadruplicates.

In this present study, the lowest crude humic substance rate (CHS1) is considered optimum rate for increasing MR219 variety rice plants’ dry matter production, uptake of N, crude Si, Ca, Mg, Zn, Cu, and Fe, and recovery of N, Mg, Zn, and Cu. However, application of crude humic substances at the rate of 40 g pot⁻¹ (CHS2) showed similar effect as that of CHS1 on plant height, number of leaves, tillers, uptake of K, P, crude Si, Ca, Mg, Na, Mn, and Zn, and recovery of P, K, and Mg.

4. Conclusions

Amending an acid soil (Typic Paleudults) with crude humic substances in waterlogged condition increased ammonia loss. However, application of the lowest crude humic substances rate (20 g pot⁻¹) improved rice plant dry matter production, nutrients uptake, recovery, and soil chemical properties. Therefore, crude humic substances could be used to amend acid soils in flooded rice fields to improve MR219 rice plant growth and soil chemical properties but long term field evaluation is essential to consolidate the findings of this study. This aspect is being embarked on in our ongoing field experiments.

Conflict of Interests

The authors declare that there is no conflict of interests regarding the publication of this paper.

Acknowledgments

Authors acknowledge Ministry of Education (MOE), Malaysia, for Long-term Research Grant Scheme LRGS (Food Security-Enhancing sustainable rice production), and Universiti Putra Malaysia for funding this research project.

References

A. R. Zaharah, H. Zulkifli, and H. A. H. Sharifuddin, “Evaluating the efficacy of various phosphate fertiliser sources for oil palm seedlings,” Nutrient Cycling in Agroecosystems, vol. 47, no. 2, pp. 93–98, 1997.

K. J. Goh and P. S. Chew, “Workshop on direct application of phosphate rocks and appropriate technology fertilisers in Asia: what hinder acceptance and growth,” in Direct Application of Phosphates to Plantation Tree Crops in Malaysia, pp. 59–76, 1995.

Y. E. Sallade and J. T. Sims, “Phosphorus transformations in the sediments of Delaware's agricultural drainageways: II. Effect of reducing conditions on phosphorus release,” Journal of Environmental Quality, vol. 26, no. 6, pp. 1579–1588, 1997.

G. V. Wilson, F. E. Rhoton, and H. M. Selim, “Modeling the impact of ferrihydrite on adsorption-desorption of soil phosphorus,” Soil Science, vol. 169, no. 4, pp. 271–281, 2004.

H. Y. Ch’ng, O. H. Ahmed, and N. M. Majid, “Improving phosphorus availability in an acid soil using organic amendments produced from agroindustrial wastes,” The Scientific World Journal, vol. 2014, Article ID 506356, 6 pages, 2014.

R. D. Delaune and W. H. Patrick, “Urea conversion to ammonia in waterlogged soils,” Soil Science Society of America Journal, vol. 34, no. 4, pp. 603–607, 1970.

W. Zhengping, O. Van Cleemput, P. Demeyer, and L. Baert, “Effect of urease inhibitors on urea hydrolysis and ammonia volatilization,” Biology and Fertility of Soils, vol. 11, no. 1, pp. 43–47, 1991.

J. L. Havlin, J. D. Beaton, S. L. Tisdale, and W. L. Nelson, Soil Fertility and Fertilizers: An Introduction to Nutrient Management, Prentice Hall, Upper Saddle River, NJ, USA, 6th edition, 1999.

X.-T. Ju, G.-X. Xing, X.-P. Chen et al., “Reducing environmental risk by improving N management in intensive Chinese agricultural systems,” Proceedings of the National Academy of Sciences of the United States of America, vol. 106, no. 9, pp. 3041–3046, 2009.

S. Moose and F. E. Below, “Biotechnology approaches to improving maize nitrogen use efficiency,” in Molecular Genetic Approaches to Maize Improvement, A. L. Kriz and B. A. Larkins, Eds., vol. 63 of Biotechnology in Agriculture and Forestry, pp. 65–77, Springer, Berlin, Germany, 2009.

A. O. Adesemoye and J. W. Kloepper, “Plant-microbes interactions in enhanced fertilizer-use efficiency,” Applied Microbiology and Biotechnology, vol. 85, no. 1, pp. 1–12, 2009.

G.-L. Tang, J. Huang, Z.-J. Sun, Q.-Q. Tang, C.-H. Yan, and G.-Q. Liu, “Biohydrogen production from cattle wastewater by enriched anaerobic mixed consortia: Influence of fermentation temperature and pH,” Journal of Bioscience and Bioengineering, vol. 106, no. 1, pp. 80–87, 2008.

O. K. Borggaard, B. Raben-Lange, A. L. Gimsing, and B. W. Strobel, “Influence of humic substances on phosphate adsorption by aluminium and iron oxides,” Geoderma, vol. 127, no. 3-4, pp. 270–279, 2005.

P. Hinsinger, “Bioavailability of soil inorganic P in the rhizosphere as affected by root-induced chemical changes: a review,” Plant and Soil, vol. 237, no. 2, pp. 173–195, 2001.

N. C. Brady and R. R. Weil, The Nature and Properties of Soils, Pearson Education, Cranbury, NJ, USA, 13th edition, 2002.

S. G. Sommer, L. S. Jensen, S. B. Clausen, and H. T. Søgaard, “Ammonia volatilization from surface-applied livestock slurry as affected by slurry composition and slurry infiltration depth,” Journal of Agricultural Science, vol. 144, no. 3, pp. 229–235, 2006.

L. Omar, O. H. Ahmed, and N. M. A. Majid, “Minimizing ammonia volatilization in waterlogged soils through mixing of urea with zeolite and sago waste water,” International Journal of Physical Sciences, vol. 5, pp. 2193–2197, 2010.

O. Latifah, O. H. Ahmed, and A. M. N. Muhamad, “Ammonia loss, ammonium and nitrate accumulation from mixing urea with zeolite and peat soil water under waterlogged condition,” African Journal of Biotechnology, vol. 10, no. 17, pp. 3365–3369, 2011.

S. Kasim, O. H. Ahmed, N. M. A. Majid, M. K. Yusop, and M. B. Jalloh, “Reduction of ammonia loss by mixing urea with liquid humic and fulvic acids isolated from tropical peat soil,” American Journal of Agricultural and Biological Science, vol. 4, no. 1, pp. 18–23, 2009.

A. A. Reeza, O. H. Ahmed, N. M. N. A. Majid, and M. B. Jalloh, “Reducing ammonia loss from urea by mixing with humic and fulvic acids isolated from coal,” American Journal of Environmental Sciences, vol. 5, no. 3, pp. 420–426, 2009.

S. Rosliza, O. H. Ahmed, and N. M. A. Majid, “Controlling ammonia volatilization by mixing urea with humic acid, fulvic acid, triple superphosphate and muriate of potash,” American Journal of Environmental Sciences, vol. 5, no. 5, pp. 605–609, 2009.

S. Rosliza, O. H. Ahmed, N. M. Majid, and M. B. Jalloh, “Reduction of ammonia volatilization through mixing urea with humic and fulvic acids isolated from palm oil mill effluent sludge,” American Journal of Environmental Sciences, vol. 5, no. 3, pp. 382–386, 2009.

P. Palanivell, K. Susilawati1, O. H. Ahmed, and N. M. Majid, “Effect of humin-urea-rock phosphate amendment on Bekenu series (Tipik Tualemkuts) soil,” African Journal of Biotechnology, vol. 11, no. 45, pp. 10317–10321, 2012.

P. Palanivell, O. H. Ahmed, K. Susilawati, and M. N. Ab Majid, “Mitigating ammonia volatilization from urea in waterlogged condition using clinoptilolite zeolite,” International Journal of Agriculture and Biology, vol. 17, pp. 149–155, 2015.

H. M. Peech, “Hydrogen-ion activity,” in Method of Soil Analysis, Part2, C. A. Black, D. D. Evans, L. E. Ensminger, J. L. White, F. E. Clark, and R. C. Dinauer, Eds., pp. 914–926, American Society of Agronomy, Madison, Wis, USA, 1965.

A. Piccolo, Humic and Soil Conservation. Humic Substances in Terrestrial Ecosystem, Elseiver, Amsterdam, The Netherlands, 1996.

K. H. Tan, Soil Sampling, Preparation, and Analysis, CRC Press, Boca Raton, Fla, USA, 2nd edition, 2005.

A. Cottenie, “Soil testing and plant testing as a basis of fertilizer recommendation,” FAO Soils Bulletin, vol. 38, pp. 70–73, 1980.

J. M. Bremner, “Total nitrogen,” in Methods of Soil Analysis, Part 2, C. A. Black, D. D. Evans, L. E. Ensminger, J. L. White, F. E. Clark, and R. D. Dinauer, Eds., pp. 1149–1178, American Society of Agronomy, Madison, Wis, USA, 1965.

D. R. Keeney and D. W. Nelson, “Nitrogen-inorganic forms,” in Methods of Soil Analysis Part 2, A. L. Page, D. R. Keeney, D. E. Baker, R. H. Miller, R. J. Ellis, and J. D. Rhoades, Eds., Agronomy Monograph no. 9, pp. 159–165, ASA and SSSA, Madison, Wis, USA, 1982.

A. Mehlich, Determination of P, K, Na, Ca, Mg and NH₄, p. S.T.D.P. no. 1–53, Soil Test Division Mimeo, North Carolina Department of Agriculture, Raleigh, NC, USA, 1953.

J. Murphy and J. P. Riley, “A modified single solution method for the determination of phosphate in natural waters,” Analytica Chimica Acta, vol. 27, pp. 31–36, 1962.

D. L. Rowell, Soil Science: Methods and Applications, Longman Scientific & Technical, 1994.

S. Paramananthan, Soils of Malaysia: Their Characteristics and Identification, vol. 1, Academy of Sciences Malaysia, 2000.

P. Palanivell, K. Susilawati, O. H. Ahmed, and N. M. Majid, “Compost and crude humic substances produced from selected wastes and their effects on Zea mays l. nutrient uptake and growth,” The Scientific World Journal, vol. 2013, Article ID 276235, 15 pages, 2013.

B. Chefetz, P. G. Hatcher, Y. Hadar, and Y. Chen, “Chemical and biological characterization of organic matter during composting of municipal solid waste,” Journal of Environmental Quality, vol. 25, no. 4, pp. 776–785, 1996.

A. C. Petrus, O. H. Ahmed, A. M. N. Muhamad, H. M. Nasir, and M. Jiwan, “Effect of K-N-humates on dry matter production and nutrient use efficiency of maize in Sarawak, Malaysia,” TheScientificWorldJournal, vol. 10, pp. 1282–1292, 2010.

O. H. Ahmed, M. H. A. Husni, A. R. Anuar, M. M. Hanafi, and E. D. S. Angela, “A modified way of producing humic acid from composted pineapple leaves,” Journal of Sustainable Agriculture, vol. 25, no. 1, pp. 129–139, 2005.

P. Palanivell, K. Susilawati, O. Ahmed, and A. N. Muhamad, “Effects of extraction period on yield of rice straw compost humic acids,” African Journal of Biotechnology, vol. 11, no. 20, pp. 4530–4536, 2012.

O. H. Ahmed, H. Aminuddin, and A. H. M. Hanif, “Ammonia volatilization and ammonium accumulation from urea mixed with zeolite and triple superphosphate,” Acta Agriculturae Scandinavica Section B: Soil and Plant Science, vol. 58, no. 2, pp. 182–186, 2008.

K. B. Siva, H. Aminuddin, M. H. A. Husni, and A. R. Manas, “Ammonia volatilization from urea as affected by tropical-based palm oil mill effluent (pome) and peat,” Communications in Soil Science and Plant Analysis, vol. 30, no. 5-6, pp. 785–804, 1999.

Muda Agricultural Development Authority, “Rice check,” 2014, http://www.mada.gov.my/semakan-tanaman-padi

Y. A. Liew, S. R. S. Omar, M. H. A. Husni, M. A. Z. Abidin, and N. A. P. Abdullah, “Effects of micronutrient fertilizers on the production of MR 219 rice (Oryza sativa L.),” Malaysian Journal of Soil Science, vol. 14, no. 1, pp. 71–82, 2010.

Y. Singh, H. C. Sharma, K. Singh et al., “Rice yield as affected by use of biofortified straw compost combined with NPK fertilizer,” International Rice Research Notes, vol. 30, no. 1, pp. 47–48, 2005.

M. Tejada and J. L. Gonzalez, “Crushed cotton gin compost on soil biological properties and rice yield,” European Journal of Agronomy, vol. 25, no. 1, pp. 22–29, 2006.

S. R. Dar, T. Thomas, I. M. Khan, J. C. Dagar, A. Qadar, and M. Rashid, “Effect of nitrogen fertilizer with mushroom compost of varied C:N ratio on nitrogen use efficiency, carbon sequestration and rice yield,” Communications in Biometry and Crop Science, vol. 4, no. 1, pp. 31–39, 2009.

S. Goyal, D. Singh, S. Suneja, and K. K. Kapoor, “Effect of rice straw compost on soil microbiological properties and yield of rice,” Indian Journal of Agricultural Research, vol. 43, pp. 263–268, 2009.

M. Tejada and J. L. González, “Application of two vermicomposts on a rice crop: effects on soil biological properties and rice quality and yield,” Agronomy Journal, vol. 101, no. 2, pp. 336–344, 2009.

T. Watanabe, L. H. Man, D. M. Vien et al., “Effects of continuous rice straw compost application on rice yield and soil properties in the Mekong Delta,” Soil Science and Plant Nutrition, vol. 55, no. 6, pp. 754–763, 2009.

A. S. F. Araújo and R. T. R. Monteiro, “Plant bioassays to assess toxicity of textile sludge compost,” Scientia Agricola, vol. 62, no. 3, pp. 286–290, 2005.

H. R. Bozorgi, A. Faraji, R. K. Danesh, A. Keshavarz, E. Azarpour, and F. Tarighi, “Effect of plant density on yield and yield components of rice,” World Applied Sciences Journal, vol. 12, no. 11, pp. 2053–2057, 2011.

Malaysian Meteorological Department, “10-Day Agrometeorogical Bulletin,” 2014, http://www.met.gov.my/

S. Yoshida, D. A. Forno, J. H. Cock, and K. A. Gomez, Laboratory Manual for Physiological Studies of Rice, LAGUNA, 3rd edition, 1976.

A. R. Dobermann, “Nitrogen use efficiency—state of the art,” in Proceedings of the IFA International Workshop on Enhanced-Efficiency Fertilizers, p. 17, Frankfurt, Germany, June 2005.

SAS, SAS/STAT Software, SAS Institute, Cary, NY, USA, 2008.

L. Bundan, N. M. A. Majid, O. H. Ahmed, M. Jiwan, and F. R. Kundat, “Ammonia volatilization from urea at different levels of zeolite,” International Journal of Physical Sciences, vol. 6, no. 34, pp. 7717–7720, 2011.

Y. Avnimelech and M. Laher, “Ammonia volatilization from soils: equilibrium considerations,” Soil Science Society of America Journal, vol. 41, no. 6, pp. 1080–1084, 1977.

D. S. Mikkelsen, S. K. De Datta, and W. N. Obcemea, “Ammonia volatilization losses from flooded rice soils,” Soil Science Society of America Journal, vol. 42, no. 5, pp. 725–730, 1978.

F. Gallardo-Lara and R. Nogales, “Effect of the application of town refuse compost on the soil-plant system: a review,” Biological Wastes, vol. 19, no. 1, pp. 35–62, 1987.

C. Yu, H. Liu, Y. Xing, N. S. Manukovsky, V. S. Kovalev, and Y. L. Gurevich, “Bioconversion of rice straw into a soil-like substrate,” Acta Astronautica, vol. 63, no. 7–10, pp. 1037–1042, 2008.

C. W. Smith and R. H. Dilday, Rice: Origin, History, Technology, and Production, Wiley Series in Crop Science, John Wiley & Sons, New York, NY, USA, 2002.

R. Kumar, N. K. Mehrotra, B. D. Nautiyal, P. Kumar, and P. K. Singh, “Effect of copper on growth, yield and concentration of Fe, Mn, Zn and Cu in wheat plants (Triticum aestivum L.),” Journal of Environmental Biology, vol. 30, no. 4, pp. 485–488, 2009.

S. Gotoh and W. H. Patrick, “Transformation of iron in a waterlogged soil as influenced by redox potential and pH,” Soil Science Society of America Journal, vol. 38, no. 1, pp. 66–71, 1974.