Upload
sambinu1
View
215
Download
0
Embed Size (px)
Citation preview
7/30/2019 Chaoui 2003 Soil Biology and Biochemistry
1/8
Effects of earthworm casts and compost on soil microbial activityand plant nutrient availability
Hala I. Chaoui1, Larry M. Zibilske2, Tsutomu Ohno*
Department of Plant, Soil and Environmental Sciences, 5722 Deering Hall, University of Maine, Orono, ME 04469-5722, USA
Received 9 November 2001; received in revised form 6 September 2002; accepted 26 September 2002
Abstract
Vermicomposting differs from conventional composting because the organic material is processed by the digestive systems of worms. The
egested casts can be used to improve the fertility and physical characteristics of soil and potting media. In this study, the effects of earthworm
casts (EW), conventional compost (CP) and NPK inorganic fertilizer (FT) amendments on N mineralization rates, microbial respiration, and
microbial biomass were investigated in a laboratory incubation study. A bioassay with wheat (Triticum aestivium L.) was also conducted to
assess the amendment effects on plant growth and nutrient uptake and to validate the nutrient release results from the incubation study. Both
microbial respiration and biomass were significantly greater in the CP treatment compared to EW treatment for the initial 35 days of
incubation followed by similar respiration rates and biomass to the end of the study at 70 days of incubation. Soil NO 32 increased rapidly in
the EW and CP treatments in the initial 30 days of incubation, attaining 290 and 400 mg N kg 21 soil, respectively. Nitrate in the EW
treatment then declined to 120 mg N kg21 soil by day 70, while nitrate in the CP treatment remained high. While ammonium levels decreased
in the CP treatment as nitrate level increased with increasing incubation time, a low level of ammonium was maintained in the EW treatment
throughout the incubation. The wheat bioassay study included two additional cast treatments (EW-N and EW2) to have treatments with
higher levels of N input. Plants grown with CP or FT treatment had a lower shoot biomass and higher shoot N content than in EW-N and EW-
2 treatments, and also showed symptoms of salinity stress. Ionic strength and other salinity indicators in the earthworm cast treatments were
much lower than in the CP treatment, indicating a lower risk of salinity stress in casts than in compost. All cast and compost amendments
significantly increased wheat P and K uptake compared to either the non-amended control or the mineral fertilizer treatment. The results
show that casts are an efficient source of plant nutrients and that they are less likely to produce salinity stress in container as compared to
compost and synthetic fertilizers.
Published by Elsevier Science Ltd.
Keywords: Earthworm casts; N mineralization; Plant nutrient uptake; Microbial respiration; Vermicomposting
1. Introduction
Vermicomposting is the digestion of organic materials by
earthworms which produce excreta known as casts.
Edwards (1995) reported that in a Rothamsted study with
25 types of vegetables, fruits or ornamentals, earthworm
casts (EW) performed better than compost or commercial
potting mixture amendments. It was suggested that the
higher crop performance of the cast treatment was due to:better soil physical structure; presence of plant growth
hormones; higher levels of soil enzymes; and greater
microbial populations. The beneficial effects of earthworm
cast utilization in other horticulture settings have also been
reported (Tomati et al., 1987; Hidalgo, 1999; Saciragic and
Dzelilovic, 1986).
EW typically have high N contents which suggests that
they would be good sources of plant N (Parmelee and
Crossley, 1988; Ruz-Jerez et al., 1992). Fresh casts often
contain high ammonium levels, but rapid nitrification results
in stable levels of both nitrogen forms due to organic matter
protection in dry casts (Decaens et al., 1999). Nutrients in
casts are initially physically protected, but this is reduced as
the aggregate structure weakens over time (McInerney and
0038-0717/03/$ - see front matter Published by Elsevier Science Ltd.
PII: S 0 0 3 8 - 0 7 1 7 ( 0 2 ) 0 0 2 7 9 - 1
Soil Biology & Biochemistry 35 (2003) 295302www.elsevier.com/locate/soilbio
1 Department of Agricultural Engineering, The Ohio State University,
250 Agricultural Engineering Building, 590 Woody Hayes Drive,
Columbus, OH 43210, USA.2
USDA-ARS, Kika de la Garza Subtropical Agricultural ResearchCenter, Integrated Farming and Natural Resources Research Unit, 2413
E. Hwy 83, Bldg 201, Weslaco, TX 78596-8344, USA.
* Corresponding author. Tel.:1-207-581-2975; fax:1-207-581-2999.
E-mail addresses: [email protected] (T. Ohno), [email protected]
(H.I. Chaoui), [email protected] (L.M. Zibilske).
http://www.elsevier.com/locate/soilbiohttp://www.elsevier.com/locate/soilbio7/30/2019 Chaoui 2003 Soil Biology and Biochemistry
2/8
Bolger, 2000). In addition to increased N availability, C, P,
K, Ca and Mg availability in the casts is also greater than in
the starting feed material (Orozco et al., 1996; Daniel and
Anderson, 1992; Lavelle et al., 1992; Basker et al., 1993).
Earthworm cast amendment has been shown to increase
plant dry weight (Edwards, 1995; Lui et al., 1991) and plant
N uptake (Zhao and Huang, 1988; Tomati et al., 1994). The
beneficial effect of EW has been observed in both
horticultural plants (Tomati et al., 1987; Hidalgo, 1999;
Saciragic and Dzelilovic, 1986) and in agronomic crops
(Pashanasi et al., 1996). Cantanazaro et al. (1998) and Cox
(1993) demonstrated the importance of the synchronization
between nutrient release and plant uptake and showed that
slower release fertilizers can increase plant yield and reduce
nutrient leaching. EW could serve as a naturally produced
slow release source of plant nutrients.Traditional composts also have agronomic value, but N
immobilization (Sims, 1990), salinity effects (OBrien and
Barker, 1996), and pathogen levels (Eastman, 1999) may be
problematic. Vinceslas-Akpa and Loquet (1997) compared
the effects of composting and vermicomposting lignocellu-
losic maple waste and reported that the vermicompost
product had a lower C/N ratio, higher protein:organic C
ratio, and higher levels of N, which indicates that the
vermicompost products were more suitable for soil amend-
ment use.
In containerized production systems, EW used as an
alternative soil amendment could help reduce several
problems associated with the use of conventional syntheticfertilizer such as excessive leaching loss of nutrients and
salinity-induced plant stress. In addition EW can improve
soil porosity, and thus provide a better root growth medium.
In this study, the effects of stabilized EW, compost and
synthetic fertilizers on soil fertility and plant growth were
investigated by determining mineralization rates of N, P,
and K; microbial biomass-C levels; and microbial respir-
ation in a laboratory incubation experiment. In addition, a
greenhouse plant growth study with wheat (T. aestivium L.)
was conducted to confirm the results of the incubation
experiment.
2. Materials and methods
2.1. Soils and materials characterization
The surface horizon of a Nicholville (course-silty, mixed,
frigid, Aquic Haplorthod) soil was obtained from the
University of Maine Sustainable Agriculture Research
Farm in Stillwater, Maine, USA. The soil contained 78%
sand, 12% silt and 10% clay fractions as determined by the
hydrometer method (Gee and Bauder, 1986). EW of
Lumbricus rubellus were obtained from the Cape Cod
Worm Farm (Buzzards Bay, Massachusetts, USA). Com-
post produced from cattle manure, leaves, and food scrapswere obtained from the University of Maine Witter
Research Farm. The particular feedstock utilized for cast
production and composting will influence the specific
chemical characteristics of the end products. However, we
believe that the materials used in this study are representa-
tive of typical EW and compost available to growers. The
compost and casts were stored at their native moisture state.
The extractable NH4-N and NO3
2-N in the soil and
amendment materials were determined by KCl extraction.Five g samples were extracted in 50 ml of 1 M KCl, placed
on a reciprocal shaker for 15 min at 200 oscillations min21.
The suspensions were filtered and analyzed for NH4-N and
NO32-N using an autoanalyzer. Nutrient contents of the
amended soil mixtures were determined by extracting 5 g
soil with 20 ml of modified-Morgan extract (1.25 M
ammonium acetate, pH 4.8), shaking for 15 min at
18 oscillations min
21
, and filtration of the suspension(McIntosh, 1969). The P, K, Ca, and Mg content of the
extract was determined by inductively coupled plasma
atomic emission spectrometry (ICP-AES). The total carbon
and nitrogen contents of the soil and amendment materials
were determined using a LECO CN-2000 analyzer (St
Joseph, MI).
2.2. Preparation of soilamendment mixtures
This study was designed to evaluate the effect of
earthworm cast and compost amendment on N release
dynamics as compared to synthetic fertilizer. The treatments
were: soil earthworm cast (EW); soil compost (CP);soil synthetic fertilizer (FT); and soil without amendment
served as a control (CT). The treatment rates utilized weredesigned to equalize the quantity of N that would be
available to the plant in a 28-day growth period. A
preliminary incubation study estimated that the N miner-
alized in 28 days were 1.5% and 1.7 of the total nitrogen
content in compost and casts, respectively. The amendment
rates were calculated taking into account the N content, the
bulk densities of the two amendments and the 530 cm3
volume of the pot. The EW treatment contained 267 g
casts kg21 soil and the CP treatment contained 189 g
compost kg21 soil. This resulted in an addition of 35% of
compost and 36% of casts by volume, which minimized theeffect of different bulk densities in the different treatments.
These amendment rates would be appropriate for contain-
erized production systems. The FT treatment received
63 mg N kg21 soil as (NH4)2SO4; 20 mg P kg21 soil as
NaH2PO4H2O; and 108 mg K kg21 soil as K2SO4. All
amendments were thoroughly mixed with the soil and
placed in three separate units: an incubation jar to determine
nutrient mineralization and microbial biomass, a respiration
flask to determine microbial respiration, and a planted pot to
bioassay N availability. The experimental design was a
complete randomized design with three replications.
Field capacity of the treatment mixtures as determined by
gravimetric draining was 42% for the soil, 55% for the CPtreatment (soil compost), 57% for the EW treatment
H.I. Chaoui et al. / Soil Biology & Biochemistry 35 (2003) 295302296
7/30/2019 Chaoui 2003 Soil Biology and Biochemistry
3/8
(soil EW), 77% for the EW-2 and 79% for the EW-N
treatment. Soil moisture levels were maintained at their
respective field capacity levels by daily watering throughout
the experiment.
2.3. Nitrogen mineralization study
The open mineralization incubation pots were placed in a
growth chamber kept at 70% relative humidity, 16 h of light
at 20 8C and 8 h of dark at 16 8C. The mineralization jars
were sampled on 3, 7, 15, 22, 28, 35, 43, 50, 57, and 70 days
after incorporation by removing 60 g of soil. Nitrogen and
other plant nutrient content was determined as described
above. Microbial biomass was determined in the soils using
a chloroform fumigation and extraction methodology
(Voroney et al., 1991). Biomass C calculations followed
Howarth and Paul (1994) using an extraction efficiency
constant of 0.35.
2.4. Microbial respiration study
The microbial respiration flasks were placed in a 19 8C
incubator. The flasks were sampled after 3, 7, 14, 22, 28, 35,
50, 57, 64, and 72 days of incubation. The alkali trap method
was used to quantify the released CO2 (Landa and Fang,
1978). The stoppered 500 ml Erlenmeyer respiration flasks
contained soil treatments at field capacity and scintillation
vials containing 10 ml of 4 M NaOH. Flasks containing the
alkali traps alone served as controls. The alkali traps were
replaced at each sampling date and titrated with 1 M HCl(Stotzky, 1965). The respired CO2 was derived from
titration data, corrected for the control.
2.5. Plant bioassay study
Seeds of winter wheat (T. aestivium L.) were briefly
rinsed with 0.525% NaOCl solution, rinsed thoroughly with
de-ionized water and germinated in a petri dish at 24 8C for
2 days prior to planting. Two seedlings were planted per pot
and placed in a growth chamber set to identical conditions
used in the incubation study above. Two treatments in
addition to those used in the N mineralization study
described above were added to the plant bioassay study:EW-2 which had an increased casts amendment rate (as
compared to EW) of 491 g casts kg21 soil (44% by volume),
and EW-N at a rate of 330 g casts kg21 soil (36% by
volume) which used a different cast lot which contained a
higher total N content than EW was used (Table 1). On day
28, the plant shoots were harvested and washed. The plantmatter was dried at 70 8C for 72 h, weighed and ground for
elemental analysis. The N content was determined using the
CN analyzer. The P and K contents were determined by dry-
ashing the plant tissue at 450 8C for 5 h and re-dissolving the
ash prior to analysis by ICP-AES.
A saturated paste extract was prepared from soil sampled
after plant harvest to determine soluble plant nutrients and
electrical conductivity of the extract. The electrical
conductivity values were converted to ionic strength using
the regression reported by Griffin and Jurinak (1973).
3. Results
3.1. Amendment materials
Although the compost material has a higher absolute N
and C content than the casts, the C/N ratios were very
similar (Table 1). The compost material had a higher level
of extractable NH4 than the casts, but both contained
comparable amounts of NO32 (Table 1). The lower levels of
NH4 found in the EW are probably due to the high
nitrification rates associated with cast stabilization (Decaens
et al., 1999). The compost contained a greater amount of
extractable K and lower amount of extractable P than theEW casts.
3.2. Microbial respiration and biomass
The average daily CO2 production is shown in Table 2.
The elevated respiration across all treatments at day 3 is
most likely due to the stimulation of the soil microbial
activity by the greater oxygen availability attributable to
physical mixing of the soil and amendments at the start of
the experiment. Respiration in the control was relatively
stable from day 7 to the end of the experiment. As shown in
Table 2, respiration levels for the CP treatment were
significantly higher than in the EW treatment for the initial35 days and they then became statistically equivalent until
Table 1
Total C and N; 0.5 M K2SO4 extractable C; 1 M potassium chloride extractable NH4-N and NO3
2-N; 1.25 M ammonium acetate (pH 4.8) extractable K and P;
and microbial biomass of the amendments and soil used in the study
Material Total N
(g kg21)
Total C
(g kg21)
C/N ratio Extractable C
(mg kg21)
Extractable NH4-N
(mg kg21)
Extractable NO32-N
(mg kg21)
Extractable K
(g kg21)
Extractable P
(g kg21)
Microbial biomass
(mg kg21)
EW 13.9 157 11.3 724 1.7 282 1.93 3.71 658
EW-N 15.8 183 11.6 1510 2.3 328 2.29 4.31 148
CP 19.6 228 11.6 5090 14.7 310 11.4 2.42 3980
Soil 3.0 39 13.0 566 4.8 19 0.27 0.01 433
H.I. Chaoui et al. / Soil Biology & Biochemistry 35 (2003) 295302 297
7/30/2019 Chaoui 2003 Soil Biology and Biochemistry
4/8
the end of the incubation. In general, microbial biomass
increased rapidly during incubation, peaking at 15 days for
both casts-treated (EW) and compost treated (CP) soils
(Table 3). The level of microbial biomass was significantly
lower in the EW treatment than in the CP treatment in the
initial 28 days which was probably due to the initially lower
microbial biomass contributed by the casts (Table 1).
3.3. Nutrient mineralization
The quantity of KCl-extractable NH4-N decreased
steadily during the entire incubation time in the FT
treatment which received (NH4)2SO4 and decreased rapidly
within the initial 15 days in the CP treatment (Fig. 1A). The
KCl-extractable NO32-N levels generally increased with
incubation time which was probably due to the transform-
ation of ammonium to nitrate (Fig. 1B). The Morgan soil
test levels of both P and K did not change during the
incubation which suggests that the content of these elements
in the amendments was sufficient for microbial growth.
Extractable P (mg P kg21 soil) in the treatments were: EW,
535; CP, 245; FT, 6.1; and CT, 5.1. Extractable K (mg
K kg
21
soil) in the treatments were: EW, 810; CP, 2830; FT,1020; and CT, 380.
3.4. Plant bioassay analysis
Plant dry shoot biomass data are shown in Fig. 2. The
EW-N, EW-2 and CP shoot weights were significantly
greater than in the EW treatment which is probably due to
higher levels of plant available N in these treatments. The
EW treatment biomass was statistically equivalent to the
NPK FT treatment and all amendment treatments signifi-
cantly increased biomass over the unamended control
treatment. The shoot N content (dry shoot weight X N
concentration) was the highest for the NPK FT treatment,followed by the CP treatment (Fig. 3). The EW-2 and EW-N
treatments had shoot N contents which were statistically
equivalent followed by the EW treatment which has
significantly lower N uptake than EW-2, but not EW-N
(Fig. 3). Shoot P content in all the EW and CP treatments
were higher than in the FT and CT treatments, demonstrat-
ing that these amendments may be adequate sources of P
(Fig. 4A). The K content results were similar with uptake
from the EW-2, EW-N, and CP treatments being higher than
from the other treatments (Fig. 4B).
4. Discussion
The elemental composition of the EW and compost
materials used suggests that the materials have potential as
alternative plant nutrient sources. The low C/N ratio
indicates that the casts and compost would be effective
sources of N through rapid N mineralization reactions
Table 2
Average soil respiration in microgram of CO2 produced per gram of dry soil per day in the earthworm cast (EW), compost (CP), fertilizer (FT) and unamended
control (CT) treatment soils during the incubation
Days EW (mg CO2 g soil21 day21) CP (mg CO2 g soil
21 day21) FT (mg CO2 g soil21 day21) CT (mg CO2 g soil
21 day21)
3 187 ba 464 a 115 b 138 b
7 63 b 324 a 39 b 35 b
14 86 b 227 a 47 c 52 c
22 44 b 186 a 39 b 48 b
28 77 b 190 a 23 c 32 c
35 82 b 155 a 21 c 25 c
50 117 a 122 a 14 b 16 b
57 71 a 76 a NDb 14 b
64 79 a 89 a 24 b 12 b
72 66 a 77 a 4 b 6 b
a Fishers protected mean separation test was used at the p , 0.05 level within each treatment. Means within a row followed by the same letter are not
significantly different.b ND, not determined.
Table 3
Microbial biomass in microgram of C per gram of dry soil per day in the
earthworm cast (EW), compost (CP), fertilizer (FT), and unamended
control (CT) treatment soils during the incubation
Days EW
(mg C g soil21)
CP
(mg C g soil21)
FT
(mg C g soil21)
CT
(mg C g soil21)
3 350 ba 730 a 140 c 183 c
7 634 b 677 a 157 b 207 b
15 653 b 973 a 404 c 175 d
22 284 bc 639 a 433 abc 179 c
28 345 b 688 a 358 ab 191 b
35 297 ab 495 a 316 ab 166 b
43 404 a 316 a 120 b 283 a
50 326 b 589 a 187 b 357 b
57 424 a 318 ab 178 b 254 b
70 397 b 866 a 121 c 272 bc
a
Fishers protected mean separation test was used at the p,
0.05 levelwithin each treatment. Means within a row followed by the same letter are
not significantly different.
H.I. Chaoui et al. / Soil Biology & Biochemistry 35 (2003) 295302298
7/30/2019 Chaoui 2003 Soil Biology and Biochemistry
5/8
(Tisdale et al., 1993). The compost material contained a
much higher level of soluble organic C (K2SO4-extractable)
than the cast materials. This is indicative of the lesser degree
of decomposition that the compost has undergone and
suggests that the material is still rich in labile carbon
compounds which can serve as an energy source for
Fig. 1. Potassium chloride (1 mol l21) extractable levels of (A) ammonium
nitrogen and (B) nitrate nitrogen during the incubation period in EW,
compost (CP), synthetic NPK fertilizer (FT), and control (CT) treatments.
Fig. 2. Total potassium chloride (1 mol l
21
) extractable (ammonium plusnitrate nitrogen) levels during the incubation period in EW, compost (CP),
synthetic NPK fertilizer (FT), and control (CT) treatments.
Fig. 3. Dry matter biomass of shoots in the earthworm cast (EW), the EW
cast at higher amendment rate (EW-2), earthworm cast with a higher native
N content (EW-N), compost (CP), synthetic NPK fertilizer (FT), and
control (CT) treatment pots. Fishers protected mean separation test was
used at the p , 0.05 level between each treatment mean. Means within a
row followed by the same letter are not significantly different.
Fig. 4. Plant shoot N uptake in the earthworm cast (EW), the EW cast at
higher amendment rate (EW-2), earthworm cast with a higher native N
content (EW-N), compost (CP), synthetic NPK fertilizer (FT), and control
(CT) treatment pots. Fishers protected mean separation test was used at thep , 0.05 level between each treatment mean. Means within a row followed
by the same letter are not significantly different.
H.I. Chaoui et al. / Soil Biology & Biochemistry 35 (2003) 295302 299
7/30/2019 Chaoui 2003 Soil Biology and Biochemistry
6/8
microbes. Casts are a byproduct of the digestion process so
they would be expected to be lower in soluble organic
compounds which are used as a microbial energy substrate.
Although the nutrient content in casts and composts are
much lower than that found in synthetic fertilizers, they are
comparable in nutrient content to that typically found in
other secondary sources such as animal manure (Troeh and
Thompson, 1993). As with other carbon-rich amendment
materials, casts and compost have the potential to increase
soil organic matter levels and improve soil quality.
The quantity of soluble C was 6.3 times greater in the CP
material than in the EW method and suggests that the initial
microbial activity is linked to the level of soluble C in the
treatments (Table 1). Likewise, the microbial activity in the
later stages of the incubation may have been controlled by
the nearly equivalent amount of total of C added to the soil(CP, 25.1 g C added; EW, 21.0 g C added). There were no
significant differences in respiration rates between the soil
amended with mineral fertilizer (FT) and the control (CT),
suggesting that microbial activity was not limited by
inadequate nutrient levels in the soil. In addition to the C
status in controlling microbial respiration, improved aera-
tion of the EW and CP treatment are also thought to be
involved. The greater pore volume in cast and compost
amended soils increases the availability of both water and
nutrients to microorganisms in soils (Scott et al., 1996).
EW may have reduced levels of microbial biomass due
the earthworm use of microbes as an energy source (Bohlen
and Edwards, 1995). Microbial biomass after 35 days of
incubation was highly variable for the EW and CP
treatments, increasing and decreasing with incubation
time. Microbial biomass in the EW treatments did not
significantly differ from the control (CT) in the four final
(Days 43, 50, 57 and 70) sampling dates (Table 3).
However, soil respiration rates for the EW treatment was
significantly higher than in the control soil in these final four
sampling dates (Table 2). The higher respiration rates in the
EW treatment in conjunction with no difference in biomass
as compared to the control could be due to the presence of
different classes of microorganisms in the casts which might
have a different respiration to biomass ratio than theorganisms found in the soil, such as the fungi observed by
Marinissen and Dexter (1990). Bohlen and Edwards (1995)
and Daniel and Anderson (1992) reported similar differ-
ences between soil microbial biomass and respiration level.
This incubation study suggests that EW could serve as a
naturally produced, slow release source of plant nutrients.
The slope of NO3-N production over time shown in Fig. 1B
corresponds to an average rate of the microbially mediated
nitrification reaction (mg NO32-N kg21 soil day21). Thegreater nitrification in the initial 28 days for the CP
treatment (12.1 ^ 0.7 mg NO32-N kg21 soil day21) than in
the EW treatment (4.7 ^ 0.3 mg NO32-N kg21 soil day21)
which was significantly different using the t-test to evaluate
regression slopes (Zar, 1984) suggests that this microbially
mediated process was higher in CP than in EW treatment.
This may be due to the organic matter being more readily
available to microorganisms in compost than in the casts
since organic matter in casts is thought to be stabilized by
the formation of a clay casing (Chan and Heenan, 1995;
Shipitalo and Protz, 1989).
The release of total extractable N (ammonium nitrate)in the EW and CP treatments compared with the NPK FT
treatment is shown in Fig. 5. The total extractable N
Fig. 5. Plant shoot (A) P content and (B) K content in the earthworm cast
(EW), the EW cast at higher amendment rate (EW-2), earthworm cast witha higher native N content (EW-N), compost (CP), synthetic NPK fertilizer
(FT), and control (CT) treatment pots. Significant differences at the 5%
level using Duncans multiple range test between treatment means are
indicated by differing letters. Means within a row followed by the same
letter are not significantly different.
Table 4
Chemical characterization of the saturated paste extracts of the soils from the plant bioassay study at harvest
Days EW (mmol l21) EW-2 (mmol l21) EW-N (mmol l21) CP (mmol l21) FT (mmol l21)
Nitrate-N 0.87 ca 0.01 d 0.04 d 2.37 b 3.44 a
Phosphorus 0.14 c 0.20 a 0.17 b 0.13 c 0.03 d
Potassium 2.0 c 1.8 c 1.9 c 21.3 a 12.1 b
Sodium 2.3 c 2.2 c 2.1 c 17.2 a 7.9 b
Ionic Strength 18.2 c 15.0 cd 14.6 d 66.1 a 62.5 b
a Fishers protected mean separation test was used at the p , 0.05 level within each treatment. Means within a row followed by the same letter are not
significantly different.
H.I. Chaoui et al. / Soil Biology & Biochemistry 35 (2003) 295302300
7/30/2019 Chaoui 2003 Soil Biology and Biochemistry
7/8
peaked at 35 days for the EW treatment and at 43 days for
the CP treatment while the FT levels were highest at the
start of the incubation and declined with incubation time.
The decrease in nitrate and in extractable total N after the
first 7 weeks is probably due to denitrification. The levels
of P and K found in the EW and CP treatments reflected
the quantity of the nutrients present in the amendment
materials (Table 1). These results show that both EW and
CP are good supplemental sources of readily available P
and K, as well as for N.
The plant study was conducted to test whether the
results and interpretations of the incubation studies were
supported using a bioassay. There was evidence of
salinity stress in the CP and FT plants with some shoots
displaying leaf tip burn. The saturated paste soil extract
analysis conducted at harvest indicated that the levels ofNO32-N and ionic strength in the CP and FT were much
higher than in the earthworm cast treatments suggests
that the burned leaf tips in the CP and FT plants at
harvest were symptoms of salinity stress (Table 4).
Nitrate-N in the EW-2 and EW-N extracts was less than
2% of that found in CP (Table 4), although the initial
extractable N levels in EW-N and EW-2 were similar to
that of compost (Table 1). This indicates a slower N
release in casts and a possible lower risk of nitrate
leaching with the use of casts as compared to compost.
The CP treatment contained the highest quantity of Kand Na in the saturated paste extract which may have
also contributed to the salinity stress in that treatment(Table 4). This result suggests that casts may be safer
than compost and water-soluble synthetic fertilizers in
containerized systems.
In summary, when sufficient quantities of casts (EW-2)
and casts higher in N content (EW-N) were used to provide
sufficient N to the plant, dry shoot biomass was greater than
the yield obtained with equivalent quantity of NPK fertilizer
and statistically equivalent to a treatment where the N
source was compost. Shoot N content was higher in the CP
and FT treatments than in any of the earthworm cast
treatments and evidence of salinity stress symptoms were
observed. These results suggest that EW in EW-2 and EW-
N resulted in higher plant biomass production due to aslower rate of nitrogen mineralization that was more
synchronized with the plant requirements (Cox, 1993).
Ionic strength and other salinity indicators in earthworm
cast treatment were much lower than in the CP treatment,
indicating that the casts used in this study did not cause
adverse salinity stress. The plant biomass and shoot
elemental content data show that casts are an efficient
source of plant nutrients and that the slower rate of N release
in EW gives it an advantage as compared to compost and
synthetic fertilizers. The nutrient content of the organic
waste fed to earthworms determines the level of nutrients
present in the obtained casts (Lavelle et al., 1992), and
compost is also affected similarly by the raw material used.However, comparable results are expected regardless of the
specific source of casts with respect to the physical structure
resulting from the gut digestive processes which is
responsible for the general slow nutrient release character-
istic of EW (Shipitalo and Protz, 1986).
Acknowledgements
Support for this work was provided by Hatch funds from
the Maine Agricultural and Forest Experiment Station.
MAFES Journal Publication 2603.
References
Basker, A., Macgregor, A.N., Kirman, J.H., 1993. Exchangeable potassiumand other cations in non-ingested soil and casts of two species of pasture
earthworms. Soil Biology & Biochemistry 25, 16731677.
Bohlen, P.J., Edwards, C.A., 1995. Earthworm effects on N dynamics and
soil respiration in microcosms receiving organic and inorganic
nutrients. Soil Biology & Biochemistry 27, 341348.
Cantanazaro, C.J., Williams, K.A., Sauve, R.J., 1998. Slow release versus
water soluble fertilization affects nutrient leaching and growth of potted
chrysanthemum. Journal of Plant Nutrition 21, 10251036.
Chan, K.Y., Heenan, D.P., 1995. Occurrence of enchytraeid worms and
some properties of their casts in an Australian soil under cropping.
Australian Journal of Soil Research 33, 651657.
Cox, D.A., 1993. Reducing nitrogen leaching-losses from containerized
plants: the effectiveness of controlled-release fertilizers. Journal of
Plant Nutrition 16, 533545.
Daniel, O., Anderson, J.M., 1992. Microbial biomass and activity in
contrasting soil materials after passage through the gut of the
earthworm Lumbricus rubellus Hoffmeister. Soil Biology & Biochem-
istry 24, 465470.
Decaens, T., Rangel, A.F., Asakawa, N., Thomas, R.J., 1999. Carbon
and nitrogen dynamics in ageing earthworm casts in grasslands of
the eastern plains of Colombia. Biology and Fertility of Soils 30,
2028.
Eastman, B.R., 1999. Achieving pathogen stabilization using vermicom-
posting. Biocycle 40, 6264.
Edwards, C.A., 1995. Historical overview of vermicomposting. Biocycle
36, 5658.
Gee, G.W., Bauder, J.W., 1986. Particle size analysis. In: Klute, A., (Ed.),
Methods of Soil Analysis. Part 1. Physical and Mineralogical Methods,
2nd ed, American Society of Agronomy, Madison, WI, pp. 383411,
Number 9 (Part 1).
Griffin, R.A., Jurinak, J.J., 1973. Estimation of activity coefficients from theelectrical conductivity of natural aquatic systems and soil extracts. Soil
Science 116, 2630.
Hidalgo, P. (1999). Earthworm castings increase germination rate and
seedling development of cucumber. Mississippi Agricultural and
Forestry Experiment Station, Research Report. 22 no. 6.
Howarth, W.R., Paul, E.A., 1994. Microbial biomass. In: Weaver, R.W.,
Angle, J.S., Bottomly, P. (Eds.), Methods of Soil Analysis Part 2:
Biochemical and Microbiological Properties, Soil Science Society of
America, Madison, WI, pp. 753773.
Landa, E.R., Fang, S.C., 1978. Effect of mercuric chloride on carbon
mineralization in soils. Plant and Soil 49, 179183.
Lavelle, P., Melendez, G., Pashanasi, B., Schaefer, R., 1992. Nitrogen
mineralization and reorganization in casts of the geophagous tropical
earthworm Pontoscolex corethrurus (Glossoscolecidae). Biology and
Fertility of Soils 14, 4953.Lui, S.X., Xiong, D.Z., Wu, D.B. (1991). Studies on the effect of
earthworms on the fertility of red-arid soil. Advances in management
H.I. Chaoui et al. / Soil Biology & Biochemistry 35 (2003) 295302 301
7/30/2019 Chaoui 2003 Soil Biology and Biochemistry
8/8
and conservation of soil fauna, Proceedings of the 10th
International Soil Biology Colloquium, held at Banglador, India,
August 713.
Marinissen, J.C.Y., Dexter, A.R., 1990. Mechanisms of stabilization ofearthworm casts and artificial casts. Biology and Fertility of Soils 9 (2),
163167.
McInerney, M., Bolger, T., 2000. Temperature, wetting cycles and soil
texture effects on carbon and nitrogen dynamics in stabilized earthworm
casts. Soil Biology & Biochemistry 32, 335349.
McIntosh, J.L., 1969. Bray and Morgan soil test extractions modified for
testing acid soils from different parent materials. Agronomy Journal 61,
259265.
OBrien, T.A., Barker, A.V., 1996. Evaluation of ammonium and soluble
salts on grass sod production in compost. I. Addition of ammonium or
nitrate salts. Communications in Soil Science and Plant Analysis 27,
5776.
Orozco, F.H., Cegarra, J., Trujillo, L.M., Roig, A., 1996. Vermicomposting
of coffee pulp using the earthworm Eisenia fetida: effects on C and N
contents and the availability of nutrients. Biology and Fertility of Soils
22, 162166.
Parmelee, R.W., Crossley, D.A. Jr., 1988. Earthworm production and role
in the nitrogen cycle of a no-tillage agroecosystem on the Georgia
piedmont. Pedobiologia 32, 355361.
Pashanasi, B., Lavelle, P., Alegre, J., Charpentier, F., 1996. Effect of the
endogeic earthworm, Pontoscolex corethrurus on soil chemical
characteristics and plant growth in a low-input tropical agroecosystem.
Soil Biology & Biochemistry 28 (6), 801808.
Ruz-Jerez, B.E., Ball, P.R., Tillman, R.W., 1992. Laboratory assessment of
nutrient release from a pasture soil receiving grass or clover residues, in
the presence or absence of Lumbricus rubellus or Eisenia fetida. Soil
Biology & Biochemistry 24, 15291534.
Saciragic, B., Dzelilovic, M., 1986. Effect of worm compost on soil fertility
and yield of vegetable crops cabbage leeks and sorghum hybrid yield.
Agrohemija 3, 343351.
Scott, N.A., Cole, C.V., Elliott, E.T., Huffman, S.A., 1996. Soil textural
control on decomposition and soil organic matter dynamics. Soil
Science Society of America Journal 60, 11021109.
Shipitalo, M.J., Protz, R., 1989. Chemistry and micromorphology ofaggregation in earthworm casts. Geoderma 45, 357374.
Sims, J.T., 1990. Nitrogen mineralization and elemental availability in soils
amended with composted sewage sludge. Journal of Environmental
Quality 19, 669675.
Stotzky, G., 1965. Microbial respiration. In: Black, C.A., Evans, D.D.,
White, J.L., Ensminger, L.E., Clark, F.E. (Eds.), Methods of Soil
Analysis, Part 2, American Society of Agronomy, Madison, WI, pp.
15501572.
Tisdale, S.L., Nelson, W.L., Beaton, J.D., Havlin, J.L., 1993. Soil Fertility
and Fertilizers, 5th Ed, Macmillan Publishing Co, New York.
Tomati, U., Grapelli, A., Galli, E., 1987. The hormone-like effect of
earthworm casts on plant growth. Biology and Fertility of Soils 5,
288294.
Tomati, U., Galli, E., Grappelli, A., Hard, J.S., 1994. Plant metabolism as
influenced by earthworm casts. Mitteilungen aus dem Hamburgischen
Zoologischen Museum and Institute 89 (2), 179185.
Troeh, F.R., 1993. Soils and Soil Fertility, Oxford University Press, New
York.
Vinceslas-Akpa, M., Loquet, M., 1997. Organic matter transformations in
lignocellulosic waste products composted or vermicomposted (Eisenia
fetida andrei): chemical analysis and 13C CPMAS NMR spectroscopy.
Soil Biology & Biochemistry 29, 751758.
Voroney, R.P., Winter, J.P., Gregorich, E.G., 1991. Microbe/plant/soil
interactions. In: Coleman, D.C., Fry, B. (Eds.), Carbon isotope
techniques, Academic Press, New York, pp. 7779.
Zar, J.H., 1984. Biostatistical analysis, Prentice-Hall, Englewood Cliffs, NJ.
Zhao, S.W., Huang, F.Z., 1988. The nitrogen uptake efficiency from 15N
labeled chemical fertilizer in the presence of earthworm manure (cast).
Advances in management and conservation of soil fauna, Proceedings
of the 10th International Soil Zoology Colloquium, Banglador, India.
H.I. Chaoui et al. / Soil Biology & Biochemistry 35 (2003) 295302302