- Open Access
Impact of soil physico-chemical properties on distribution of earthworm populations across different land use patterns in southern India
© The Author(s) 2018
- Received: 18 July 2018
- Accepted: 7 November 2018
- Published: 27 November 2018
The distribution of earthworms is usually diverse and their population fluctuates in relation to the different physico-chemical properties and land use patterns of the soil of southern parts of India. This particular study examined distribution and relative abundance of earthworms under different land use patterns and their influence on the physico-chemical properties of the soil. We measured the species composition of earthworm communities across the three different land use ecosystems and effect of abiotic factors on them from various ecological regions of southern India (southern Odisha).
The linear relationship between different physico-chemical parameters of soil across three land use types and earthworm density is obtained by Pearson correlation analysis in the months of June to September. The association of physico-chemical parameters of different habitats with earthworm populations is analyzed using two-way ANOVA. Principal component analysis is (PCA) used to characterize the effect of different soil properties on the distribution of earthworm populations across three different habitats.
A total of ten species of earthworms belonging to five families were identified. Four species of earthworms are identified, i.e., Pontodrilus bermudensis, Parionyx excavates, Pheretima alexandri, Lampito mauritii, most abundantly in forest lands, while the other six species are mostly found in agriculture and grass land. The earthworm density is significantly correlated (P < 0.01) with the availability of organic OC, total nitrogen, phosphorus, and water holding capacity across the three habitats, the forest land in particular. Both ANOVA and PCA results revealed a significant impact of habitat conditions on the soil physico-chemical properties as well as earthworm density.
This particular study has provided new information regarding the influence of different earthworm population on abiotic factors of soil across three land use patterns. It is also noticed that the distribution of earthworm was higher in forest lands and followed by grasslands having high organic manure rather than agricultural land.
- Landuse patterns
- Habitat preferences
- Soil abiotic factors
Earthworms constitute the largest biological component of the soil among all animal biomass in soil and are commonly referred as ecosystem engineers (Blouin et al., 2013). Earthworms are considered to be the most important soil animals in many Indian subcontinental habitats. This consideration is based on their high density as well as their severe contribution to ecological and agronomical important aspects. Earthworms are one of the principal components of the invertebrate community in most soils, both in terms of their contribution to gross belowground biomass and their effects on soil biogeochemical cycles (Bohlen, Parmelee, McCartney, & Edwards, 1997; James, 1991; Lee, 1985).
The soil physico-chemical characteristics like pH, organic matter, nitrogen (N), phosphorus (P), etc. are influenced by earthworms due their participation in the association of the soil particles, as well as in organic matter transfer. The earthworms speed up N mineralization from organic matter, which sometimes depends on the specific species and their interaction with soil characteristics, organic matter geographical position. (Butenschoen, Ji, Schaeffer, & Scheu, 2009). Hence, it is necessary to identify taxonomically those species which can survive tropical agroecosystems and significantly influence soil processes through intense activity toward a productive and sustainable soil ecosystem across various habitats (Lavelle, 1988).
There are many research works carried out across the globe which investigate the relationship between the activity of earthworms, the soil properties and environmental factors and have reported the increasing importance of earthworms. Various ecological studies have reported the close relationship between the availability of different earthworm species and various land use patterns (Nunes, Pasini, Benito, & Brown, 2006; Tao et al., 2013). The distribution of earthworms is usually diverse and their density fluctuates in connection with the abiotic factors and land use patterns of the soil as well. The distribution of earthworm is usually heterogeneous (Guild, 1952; Satchell, 1955; Svendsen, 1957) and their numbers fluctuate in change in the abiotic factors of soil (Evans & Guild, 1947). Environmental factors like temperature, pH, soil texture, and water content of soil also affect the distribution of earthworms. Bhadauria and Ramakrishnan (1989) reported that biotic and abiotic factors in particular soil properties, surface vegetation type, surface litter inputs, local/regional climate, human interference, and dynamic land management influences the regional earthworm biodiversity and species dispersal pattern. The diverse soil habitats have significant influence on factors affecting the complete earthworm distribution (Rajkhowa, Bhattacharyya, Sarma, & Mahanta, 2014). Change in land use patterns (habitats) has direct consequences on the composition and population distribution of earthworm communities in various agro-climatic zones (Behera, Dash, & Senapati, 1999; Bhadauria, Ramakrishnan, & Srivastava, 2000; Blanchart & Julka, 1997; Lalthanzara, Ramanujam, & Jha, 2011). The association among biotic and abiotic factors, earthworm activities, climate change, and land use management practices are diverse and interrelated.
Indian earthworm fauna is composed of native species, which constitute about 89% of total earthworm diversity in the country (Julka & Paliwal, 2005). The distribution of earthworm’s population is affected by various land use system, soil water content, soil organic matter, rainfall pattern, etc. Many workers studied the habitat preference of various earthworm species (Bennour & Nair, 1997; Singh, 1997; Singh, Singh, & Vig, 2016). The presence or absence of a species particularly in a habitat and its non-appearance at some other habitats indicates the species-specific distribution of earthworms in different pedoecosystems (Tripathi & Bhardwaj, 2004). Species vary in their ability to digest organic residues and assimilation of nutrients (Lattaud, Locati, Mora, & Rouland, 1998).
Agricultural activities such as irrigation, tillage, lime application, pesticide use, drainage, and crop rotation can have influence on earthworm biomass and activity (Edwards & Bohlen, 1996). Use of chemical substances such as solid materials and organic fertilizers obtained from plants and animal origins described to increase the populations of earthworm (Leroy, Schmidt, Van den Bossche, Reheul, & Moens, 2008; Leroy, Van den Bossche, De Neve, Reheul, & Moens, 2007; Reinecke, Albertus, Reinecke, & Larink, 2008). In agriculture, performance of various activities by soil organisms like control of local microclimate, recycling of nutrients, and detoxification of chemicals regulate the density of unwanted soil fauna. The increase of earthworm populations in different forest soils has been limitedly explored. The impact of local anthropogenic activities, forest and soil physico-chemical properties on earthworm abundance with community composition is also an important consideration for future forest ecosystem. The resultant effect of forest ecosystem/cover is that it improves the water stable aggregates of the soil, more particularly in degraded lands which makes the earthworms living in suitable atmosphere. The incorporation of vegetation such as green manure in forest improves the physical and chemical properties of soil (Sharma & Yogender, 2004).
More research works are therefore needed to explore the unique soil earthworm habitats from southern parts of Odisha, India since this region represents an emerging area for the studies of physiological limits of invertebrate groups of soil macro faunal and their mechanisms of action toward sustainable agricultural improvement and for human welfare. To explore and characterize unexplored earthworm fauna is essential to study the diverse soil habitats such as soil texture of various habitats, agricultural soil, forest areas, grass land soil, etc., which would bring out some new valuable findings about the soil earthworm diversity and their distribution patterns across various habitats. There is also a need of distribution pattern of earthworms, as well as the factors affecting their distribution and modification of soil health by them. This paper addresses the present state of knowledge on earthworms’ impacts on different soil structure and soil physico-chemical properties such as organic carbon (OC), pH, N, water holding capacity (WHC), P, and cation exchange capacity (CEC) with special emphasis on the effects of land use practices at different habitats. The present research work is the first to report about the effect of specific abiotic components of soil on the distribution and density of earthworm species from various habitats of agro-climatic zones of Odisha, India. We have studied those factors which have influenced earthworm species diversity and community structure in agricultural fields, forest lands, as well as grass lands.
The aim of the present study is to determine the basis of distribution and relative abundance of variety of earthworm populations under different land use patterns and its relation with the physico-chemical properties of the soil. Here, we report the results of our study in which we measured the density and species composition of earthworm communities across three different land use ecosystems from various ecological regions of southern parts of Odisha, India.
Study site and sampling
Description of study sites with latitude, longitude, and type of habitat
N 19° 37′ 16.1414″
E 83° 29′ 55.49″
Ramanaguda range, Rayagada
N 19° 12′ 384231″
E 83° 40′ 23.73″
Royat colony, Rayagada
N 19° 10′ 527″
E 83° 24′ 28.127″
N 19° 21′ 33.07″
E 84° 58′ 25640″
Mujagada forest range, Ganjam
N 19° 55′ 57.8406″
E 84° 35′ 1.759″
N 20° 25′ 26.5436″
E 85° 55′ 10.53768″
N 18° 44′ 46.1526″
E 82° 47′ 38.50728″
N 18° 45′ 52.63272″
E 82° 52′ 39.13896″
N 18° 48′ 48.5532″
E 82° 42′ 44.39772″
N 19° 3′ 40.41216″
E 83° 49′ 27.48036″
N 18° 46′ 54.17832″
E 83° 25′ 36.30648″
N 18° 46′ 41.75256″
E 84° 5′ 37.23756″
Experimental sites of different districts of Odisha, India.
Physico-chemical parameters analysis
Total nitrogen presumed equal to and measured using the total Kjeldahl method (Bremner, 1996), assuming limited mass of nitrite/nitrate because little amount of fertilizer is applied to the sampling locations. OC is measured using the Walkley-Black method (Nelson & Sommers, 1996). The pH is determined in a media water suspension (1:1 w/v) using a glass cathode microprocessor pH meter (Hanna Instruments pH 210). pH-buffered CEC measurement is done at pH 7.0. Ammonium acetate procedure of Chapman (1965) followed for the estimation of CEC. P concentration of the soil sample is estimated by colorimetric method. Soil water content is estimated by keeping fresh soil samples in an oven drying at 105 °C until constant weight. WHC is measured by using sintered crucibles filled with oven dried and sieved through 2 mm mesh soil samples kept over a container filled with water and kept for 24 h.
The linear relationship between different physico-chemical parameters of soil and earthworm density is obtained by Pearson correlation analysis. The association of physico-chemical parameters of various habitats with earthworm populations is analyzed using two-way ANOVA. All the experiments were done with n = 5 repetitions from each sampling site. Principal component analysis (PCA) is used to characterize the effect of different soil properties on the distribution of earthworm populations across three different habitats. All the analyses are done with the help of SPSS 17 software program.
Morphological characteristics of earthworm populations collected
Name of the species
Clitellum length (mm)
Average body weight (g)
Physico-chemical parameters of soil habitats of southern parts of India
C (mg g−1)
N (mg g−1)
CEC (meq/100 g)
18.4 ± 2.47
10.1 ± 0.54
1.04 ± 0.11
6.6 ± 0.35
25.44 ± 4.69
24.16 ± 0.91
6.2 ± 0.83
30.2 ± 2.44
15.6 ± 0.74
1.34 ± 0.054
6.72 ± 0.19
30.46 ± 3.53
28.70 ± 2.03
16.2 ± 1.48
23 ± 1.04
13.5 ± 0.79
1.16 ± 0.054
6.68 ± 0.23
28.15 ± 3.57
24.53 ± 2.24
16 ± 1
16 ± 1.96
10.1 ± 0.41
0.86 ± 0.054
6.52 ± 0.28
20.84 ± 2.30
23.92 ± 0.52
7.6 ± 1.14
28 ± 0.73
15.3 ± 1.44
1.28 ± 0.13
7.02 ± 0.36
30.32 ± 3.46
29.50 ± 0.90
23 ± 2.23
17.2 ± 2.32
11.9 ± 0.96
1.04 ± 0.11
6.74 ± 0.18
23.72 ± 2.46
25.03 ± 0.78
15.6 ± 2.70
12.6 ± 2.32
11.5 ± 0.79
1.02 ± 0.08
6.48 ± 0.44
20.42 ± 4.89
25.86 ± 1.77
8.4 ± 1.14
21 ± 2.24
14.5 ± 1.06
1.22 ± 0.083
6.74 ± 0.23
28.64 ± 3.18
28.83 ± 1.02
22.2 ± 1.48
15.8 ± 1.84
12.6 ± 0.96
1.08 ± 0.083
6.7 ± 0.25
23.89 ± 3.91
25.51 ± 1.18
13.6 ± 1.14
11.2 ± 1.19
11.6 ± 0.74
1.02 ± 0.13
6.42 ± 0.31
22.57 ± 3.94
23.69 ± 1.19
8 ± 1.58
16.6 ± 2.03
14.6 ± 0.96
1.2 ± 0.07
6.92 ± 0.33
29.55 ± 2.40
28.51 ± 0.74
22.4 ± 1.81
15 ± 1.12
12.6 ± 0.41
0.96 ± 0.11
6.78 ± 0.19
26.74 ± 4.27
24.30 ± 1.12
14.2 ± 1.92
Correlation between earthworms and soil physico-chemical properties across three habitats
Correlation coefficient (r) of earthworm density with soil carbon, total nitrogen, pH, phosphorus, WHC, and CEC across three different habitats
Principal components and eigenvalues with total and cumulative variance of soil factors
Total variance (%)
Analysis of variance of earthworm population with respect to soil physico-chemical parameters of different habitats
Physico-chemical parameters of various land use patterns df: degrees of freedom ANOVA (n = 5)
Physico-chemical properties of soil
Water holding capacity
Cation exchange capacity
Principal component analysis
In many regions, the type of vegetation is the major biotic factor which directly influences the distribution and diversity of earthworms in the soil (Ramanujam, Roy, & Jha, 2000). The earthworms population vary in size ranging from only few individuals (sometimes totally absent) to more than 1000/m2, which depends on the physico-chemical characteristic of the soil and the climatic (Kale & Karmegam, 2010; Lee, 1985). The change in soil texture and characteristic can influence the population of earthworm. Thus, they can serve as best indicators of several changes/factors associated with soil. Management of soil conditions can thus influence soil properties by affecting aggregation directly or indirectly to earthworm abundance and their subsequent contribution to change in soil structure.
The population of earthworm species and relative significance of different ecological categories are affected by the type of vegetation, abiotic factors, and the soil characteristics (Lavelle & Spain, 2001). Soil aggregate stability was primarily specific in relation to different land use patterns and subsequently affected by earthworm activity within their ecosystem. However, many studies have examined both anthropogenic and environmental controls on earthworm populations in agricultural systems, forest land, and grass land. Soil degradation is also associated directly with the decreases in abundances and diversity of earthworm population and other invertebrate communities (Lavelle, 1997; Lee & Foster, 1991). Tripathi and Bhardwaj (2004) reported high species richness in agricultural lands but in our study, species richness was very low (11.2 ± 1.19) in cultivated lands. The difference may be due to type of soil and agricultural practices followed at different regions. The reorganization of soil structure with the movement of earthworm through the soil and also during gut transit influences the physico-chemical properties of soil. The distribution of earthworm is usually heterogeneous (Guild, 1952; Satchell, 1955; Svendsen, 1957) and their population densities fluctuate in relation to the abiotic factors of the soil (Evans & Guild, 1947). Bhadauria and Ramakrishnan (1989) reported different biotic and abiotic forces such as soil properties, surface litter inputs, local or regional climate, dynamic land management history, surface vegetation type, and human pressure at an extent are some of the major causes which effects the regional earthworm biodiversity and species dispersal pattern. Diverse soil habitats are the most direct influencing factors that are affecting the overall earthworm distribution in a particular ecological zone (Rajkhowa et al., 2014). Changes in different land use patterns have also directly affected the composition and population structure of earthworm communities in different agro-climatic regions (Behera et al., 1999; Bhadauria et al., 2000; Blanchart & Julka, 1997; Lalthanzara et al., 2011).
Name of the species with sampling sites and habitat types
No of samples
11.61 ± 2.31
20.36 ± 2.22
14.8 ± 1.54
20.4 ± 2.45
28.2 ± 2.24
Royat colony, Rayagada
23 ± 1.54
20.4 ± 2.42
22.2 ± 2.11
23 ± 1.24
22.3 ± 1.36
Mujagada forest, Ganjam
21.7 ± 1.73
18.2 ± 2.41
20.8 ± 1.43
Buguda forest, Ganjam
18.2 ± 2.12
14.3 ± 1.22
15.2 ± 2.62
22.2 ± 2.24
Gunupur colony, Rayagada
16.5 ± 1.87
13.7 ± 1.23
15.3 ± 2.53
17.2 ± 1.42
22.35 ± 2.22
20.2 ± 2.21
17.8 ± 1.27
12.33 ± 1.23
18.34 ± 2.53
15.95 ± 1.93
18.6 ± 2.61
Polosara forest, Ganjam
20.3 ± 1.82
21 ± 1.33
These species represent two anecic, four endogeic, and four epigeic species. The overall frequency of occurrence varies: Pheretima alexandri was least frequently found (18 sites) and Lampito mauritii most frequently (70 sites), followed by Pontodrilus bermudensis (55 sites). Exotic species like Octochaetona surensis and Pontoscolex corethrurus and native peregrine species like Lampito mauritii that are widely distributed in southern parts of India (Odisha) area appear to be better adapted to withstand drought conditions, as they have enteronephricmeronephric excretory system, i.e., excrete their urine into the gut, for conservation of water in their bodies (Lee, 1985). The most common earthworm species in almost all the observed habitats across all the agro-climatic zones of Odisha were Lampito mauritii and Pontodrilus bermudensis. The presence of a species in a particular habitat and its absence from other habitats shows the species-specific distribution of earthworms in different pedoecosystems. A study conducted by Bossuyt, Six, and Hendrix (2006) showed that there was a significant influence of earthworm activity and residue application on stable aggregate formation. Further, in the presence of Eudrilus eugeniae, soil aggregates were three times greater than the control. During the survey only Lampito mauritii and Parionyx excavates anecic species and Pontoscolex corethrurus endogeic species found in North Eastern Ghat of Odisha, India. This showed that the soil layers of more than 30 cm deep were not suitable for propagation of earthworms. The earthworm fauna of southern Odisha, India are of all types belong to epigeic, endogeic, epi-anecic, endo-anecic, or anecic in nature. Edwards and Lofty (1977) suggest that earthworm species generally have narrow range in pH, very few restricted to slightly acidic soils. Most of them prefer neutral soils, but some can tolerate acidic or alkaline soils. The pH values recorded in the present study are within the range for the distribution of earthworms. Eudrilus eugeniae and Octochaetona serrata inhabited cultivated soils while Eisenia fetida and Perionyx gravely found in non-cultivated soil, reflecting a clear cut species-habitat relationship. The occurrence of Eudrilus eugeniae and Octochaetona serrata in cultivated soil might relate to higher N concentration. The earthworm species in grassland were Eisenia fetida, Pontoscolex corethrurus, and Perionyx gravely which were only present in grassland having high OC. The greater accumulation of litter on the surface soil of both agricultural and forest systems could provide sufficient space, food, shelter, and protection from predation of other animals to earthworm populations which also helps in enhancing the earthworm diversity (Ruan, Li, & Zou, 2005) in the particular soil habitat conditions. Landscape structure and species-specific dispersal and colonization abilities may also have played a crucial role in population distribution among three habitats (Decaens & Jimenez, 2002; Thomas, Folgarait, Lavelle, & Rossi, 2004).
Principal component analysis (PCA) was used in order to study the interaction between physico-chemical soil parameters and earthworm communities of studied sites. PCA resulted in five principal components viz. PC1, PC2, PC3, and PC4 contributing variances of 28.058, 25.698, 23.471, and 21.446 respectively (Table 5). This procedure makes it possible to group or distribute the sampling sites around principal axes in function of the physico-chemical and earthworm parameters, thus facilitating observation of possible links between variables and places where they are most represented (Figs. 8, 9, and 10).
Modern agricultural practices are leading to alter the physical and chemical structure of soil environment subsequently modulating the changes in abundance and composition of earthworm population (Curry, Byrne, & Schmidt, 2002) similar to this, Dale and Polasky (2007) mentioned that in agricultural systems, changes in land use patterns are the direct result of different practices of soil. Moreover, the use of pesticides and herbicides in intensive agricultural lands are going to affect earthworms in a way like from gene expression and physiology, to the individual as well as population distribution (Pelosi, Barot, Capowiez, Hedde, & Vandenbulcke, 2014; Santadino, Coviella, & Momo, 2014). Soil erosion in agricultural lands is one of the major threat to food security (Amundson et al., 2015). Agricultural practices leads to such a huge disturbance for many native earthworm species (James & Hendrix, 2004) that even after agricultural abandonment native species may not be able to repopulate secondary forests at those regions. Tripathi and Bhardwaj (2004) reported high species richness in agricultural lands since in our study species richness was very low in cultivated lands, so the difference may be due to type of soil and agricultural practices at the concerned experimental sites. Changes in vegetation can also affect the distribution and earthworm population with change in litter quality and also through soil properties (Muys & Granval, 1997).
In the present study, Eudrilus eugeniae, Octochaetona serrata, and Octochaetona surensis have been abundantly found in agriculture soil due to its endogeic ecological category which protects it directly from the effects of insecticides and pesticides and mechanical disturbance produced during agriculture practices. More plowing in agriculture field positively influence endogeic species by increasing organic matter availability and opposite effect from anecic species (Capowiez et al., 2009; Ernst & Emmerling, 2009; Metzke, Potthoff, Quintern, Heß, & Joergensen, 2007). Diversity of epigeic species like Lampito mauritii and Perionyx excavates in agricultural field was low may be due to physical disturbance of the soil during plowing and intensive use of insecticide and pesticide. The significant effect of experimental sites has been well examined on endogeic and anecic populations. Jouquet et al. (2010) also reported that endogeic earthworms are the most resistant earthworm recorded in disturbed soil. This burrowing nature of earthworm protects it from effects of insecticides and pesticides and also the mechanical pressure produced during agriculture management practices by the humans. However, there is no significant effect of different irrigation and cropping practices on epigeic abundance. Cultivated soils usually have low organic matter compared with native ecosystem for earthworm, since agricultural activities increases aeration of soil which enhances the decomposition of soil organic concentration subsequently. The differences in agricultural management practices that affect the population density and biomass of earthworm were also observed by Amador, Winiarski, and Ramirez (2013). This difference in earthworm population density across various soil habitat conditions might attribute to change in vegetation patterns in some specific experimental sites. It is also observed that the earthworm abundance is directly influenced by the management practices of agricultural lands. Thus, understanding the influence of agricultural management on earthworms and their relationship with soil organic matter dynamics is imperative for the development of sustainable agroecosystems.
Disturbance and degradation of natural forests leads to change in earthworm population structure and distribution reported by Baretta, Brown, James, Bran, and Cardoso (2007) and Chandran, Sujatha, Mohan, Julka, and Ramasamy (2012) in both the tropical and temperate regions of the soil ecosystem around the world. Bohlen et al. (2004) studied that reductions in soil C:N ratios caused by earthworm invasion of previous uncolonized forest soils. The diversity and distribution of earthworm populations is also studied by Haokip and Singh (2012) from disturbed and undisturbed subtropical forest ecosystems of Imphal, Manipur, India. Joshi and Aga (2009) made a similar kind of investigation on diversity and distribution of earthworm populations in some of the subtropical forest ecosystems of Uttarakhand, India in which they reported temperature, water content of soil, oxidizable organic matter, pH, phosphorous, potassium, calcium, and N as the potential factors influencing the diversity and distribution patterns of earthworm populations. In our study, species such as Pontodrilus bermudensis, Parionyx excavates, Pheretima alexandri, and Lampito mauritii were found abundantly in the forest areas of various habitats of districts viz. Rayagada, Ganjam, Koraput, and Gajapati (Table 1). Matson, Parton, Power, and Swift (1997) studied that the different species and their population density in the soil in tropical agricultural lands are less than 50% of that of the primary forest on that land. Agricultural conversion continues to threaten the tropical forests at some extent. Various studies reported that the disturbance and degradation of natural forest affect the number of earthworms and their distribution (Baretta et al., 2007; Chandran et al., 2012). Ayuke et al. (2009) reported that some earthworm groups which are found abundantly in the forest soils noticed positively correlated with N.
The distribution of different earthworm species is studied in various habitats of agro-climatic zones of Odisha, India. Eisenia fetida, Pontoscolex corethrurus, and Perionyx gravely were found in grassland ecosystem. Reasons for the dominance of natives in these pastures may be related to the land use history in the region, particularly its more recent colonization and the widespread use of native pastures in most of the regions. In few sites of grasslands, no earthworm was found at all. This is readily explained by the very sandy (90 to 98% sand) and nutrient-depleted soils in this site (Boeger, Wisniewski, & Reissmann, 2005). These sandy soils, in the lower horizons at the high ground water level creates anoxic situations and the upper horizons dry out quickly because of drainage, both of which are fatal for earthworm population. The lack of available nutrients (organic matter) at this depth is because of relatively low input (litter fall) from the sparse plant cover, and very irregular distribution of litter in the younger stages (Pinto & Marques, 2003) might negatively influence earthworm abundance (Lee, 1985).
Epigeic species observed 18% and 10% in permanent grasslands and agricultural land, respectively. The anecic species noticed 23% and 15% in permanent grasslands and agricultural land, respectively. The distribution of the different ecological categories of earthworms in arable land and permanent grasslands showed a preference of endogeic species, as soil dwellers with horizontal burrows. However, the numbers of endogeic species was found higher in grasslands than in agricultural land. Particularly in grasslands, the correlation between earthworm characteristics (earthworm density and distribution) and soil physico-chemical properties was not so much (Table 4). These are usually much abundant in grassland in comparison with in agricultural land, which is probably due to number of factors among which lesser availability of food and regular soil tillage in agricultural lands may be the most important causes (e.g., Barley, 1961; Boag, Palmer, Neilson, Legg, & Chambers, 1997; Edwards & Bohlen, 1996; Edwards & Lofty, 1979; Evans & Guild, 1948; Tischler, 1955; Zicsi, 1969) An exception to this is the position of the abundance of epigeic species, located close to that of Lumbricus rubellus, reflecting the dominance of this species in this ecological group. This may be regarded as an indication that the management type is important in determining the abundance in which earthworm populations occur. In particular, the higher amount of soil organic matter in grassland farms, and the less intensive soil cultivation may be decisive in this respect. The porosity of the upper layers decreased when the land used for pasturage particularly.
Change in organic carbon and total nitrogen
The significant correlations observed between earthworms and total OC and N amount contained within some of the fractions on a gm2 basis (e.g., micro-aggregates) may be because of the relationship between earthworms and the concentration of C and N in the whole soil, since the enrichment of the bulk soil would be associated with increases in C and N concentrations for at least some of the aggregate fractions comprising the whole soil. It is also observed the existence of positive correlation between OC and N, OC and earthworm population and distribution. The similar kind of results, i.e., positive correlation observed between earthworm density and total soil C and N (Blanchart et al., 1999; Shipitalo & Le Bayon, 2004). Some other studies (Kale, 1998; Sathianarayanan & Khan, 2006) have also shown the high earthworm population density associated with high C and N ratio. It shows that earthworms prefer to live in soil ecosystems rich in organic matter and N. The present observations are more or less in agreement to the findings of other workers (Appelhof, 1981; Edwards & Lofty, 1977; Hallatt, Viljoen, & Reinecke, 1992; Lavelle, 1974; Lee, 1985).
It is the relative values OC and N that affect the earthworm population. Soil C in forest soils in our study was significantly higher (P < 0.01) than grassland but the latter was significantly higher (P < 0.05) than agricultural land (Table 4). The species available at these sites are Eudrilus eugeniae and Perionyx excavates. Curry, Byrne, and Boyle (1995) noticed the contribution of earthworms by addition of 3.4–4.1 g of mineral nitrogen to the soil through excretion, mucus production, and soil ingestion in soil ecosystem. Selvakumar and Umamaheswari (2003) have also observed similar kind of results while analyzing the N concentration of the vegetable wastes composted by the earthworm species Eudrilus eugeniae. It also reported that the increased N concentration may be because of release of nitrogenous metabolic products through earthworm Eudrilus eugeniae excreta, urine, and mucoprotein components (Padmavathiamma, Li, & Kumari, 2008). Indeed, Dash et al. (1977 & 1979) studied the presence of higher levels of N in the casts of Lampito mauritii species than in the surrounding soil. Burtelow, Bohlen, and Groffman (1998) and Fonte, Thaiis, and Six (2009) observed the positive correlation between earthworm biomass with total soil OC and OC is positively correlated with distribution of earthworm. In our study, the N was positively correlated with the OC as well as P and WHC at some extent as overall. The bulk density of soil also differed in different sites. These correlations explain that soil fertility has a crucial role in the participation of earthworm that plays positive role across the soil ecosystem.
Coleman, Reid, and Cole (1983) observed the uptake of microorganisms like bacteria and fungi followed by grazing of microorganisms by the earthworms, excretion and decomposition resulted in release of P compounds which can be cycled through plants and again back to the soil. Similar kind of results were observed by Mansell, Syers, and Gregg (1981) with regard to the increase of short-term plant availability of P derived from plant litter by two- or threefold by the earthworms. The earthworm has some impacts on P dynamics and availability in the soil atmosphere depending on the physico-chemical properties of soil, as well as organic P source, and the burrowing behavior of earthworm (Bunemann, Oberson, & Frossard 2011). In the present study, P was positively correlated with soil OC, N, and WHC and observed highest in forest land then grass land and agricultural land. The mineralization of phosphate also increased P concentration (Garg, Gupta, & Satya, 2006; Kumar, Bhargava, Prasad, & Pruthi, 2015). Study by Chaudhuri, Pal, Bhattacharjee, and Dey (2000) and Vinotha, Parthasarathi, and Ranganathan (2000) noticed that increase in available phosphorous concentration in worm-worked substrate is probably because of mineralization and mobilization of phosphorous by combined action of microbial activity in casts and also the fecal phosphatase of earthworms.
Change in pH
The average pH value of soil in the study area was slightly acidic but very close to the neutral status that indicates a good pH (6.42 ± 0.31 to 7.02 ± 0.36) status and the existing pH value is positively correlated with the earthworms’ distribution. A negative correlation of pH and P with earthworm number and biomass was observed by Iordache and Borza (2010). They also found that the phosphorous concentration of soil exerted has the greatest negative influence on earthworm biomass. The change in pH toward neutrality may due to the mineralization of N and P into nitrites or nitrates and orthophosphates (Kaviraj & Sharma, 2003a, b). Chaudhuri and Bhattacharjee (1999) reported that earthworms are mostly distributed in a pH range of slightly acid to moderate alkaline, thus pH value recorded in the present study are within the range for the distribution of earthworms.
Earthworm population is available much in the soils with neutral pH. The majority of species are in distribution range between pH of 6.0 and 7. 8. The pH may increase due to high solubility of nutrients in some earthworm casts (Barley, 1959). This could be another reason for the rise in pH of the substrates in our study. In the present study, decrease in pH (6.5) observed significantly (P < 0.05) in many sites of agricultural land. The decrease in pH could also be due to production of CO2, ammonia, NO3−, and organic acid during casting process as hypothesized by Yadav, Tare, and Ahammed (2010) and Song, Liu, Wu, Lin, Ye, Jiao, and Hu, (2014).
The pH and CEC found negatively correlated across agriculture and grass land. Soil pH for agriculture soils was significantly lower than for forest soils but the latter was significantly lower than for grassland. Significant increase in soil pH after inoculation of different species of earthworms in culture medium corroborates the reports of Basker, Kirkman, and Macgregor (1994). Darwin (1883) and Lee (1985) noticed that the reason behind the change could be the fact that different species of earthworms, including Lumbricus terrestris, secrete calcium carbonate by their calciferous glands. The pH values measured in our study observed to be lower may be because of the fields used with urea ammonium nitrate fertilizer added frequently. At some experimental site in the forest habitat, a higher pH value in fresh earthworm cast compared with adjacent soil was observed. The higher pH of cast soil may be due to the ammonia secreted in the worm’s gut. In this study, soil pH tends to increase in the agricultural lands. The pH values of natural forest, grassland, and agricultural lands varied significantly 7.02 ± 0.36, 6.78 ± 0.19, and 6.60 ± 0.35 (Table 3), and natural forest and cultivated land were more acidic than those of pasture land. However at few experimental sites of agricultural land, soil pH was slightly increased with soil depth due to accumulation of basic cations. Lime concentration in forest and grassland soil was similar while lime concentration significantly increased under agricultural land. More or less a negative correlation was found between pH value of soil and earthworm species distribution in different habitats.
Variation in WHC
WHC in soils is primarily controlled by the pore-size distribution of soils and also the number of pores with specific surface area in a selected area. This suggests that increase in soil organic concentration with increased aggregation and decreased bulk density leads to increase the total pore space as well as the number of small pore sizes in a given area (Haynes, 2000; Khaleel, Reddy, & Overcast, 1981). Generally, earthworm casts have a higher range of water holding capacity in comparison to bulk soils (Elliot, Knight, & Anderson, 1990). In our study, forest soil of almost all district showed highest WHC ranges from 28.51 ± 0.74 to 29.50 ± 0.90. The species present at higher WHC were Octochaetona surensis and Octochaetona serrate. These results are similar with the findings of Abbott and Parker (1981), who reported an increased infiltration of water due the activity of the geophagous earthworm species Microscolexdubuis in the presence of clover mulch. They also declared that decreased infiltration in grass plots were probably because of fine roots clogging soil pores.
Hence, our results suggest that the presence of grasses and legumes at the study areas affected the hydraulic conductivity through various mechanisms directly with root activity and indirectly through earthworm biomass alteration. Ehlers (1975) and Bouche (1977) reported that macropores formed by earthworms between 2 and 11 mm in diameter depends on the presence of ecological group of earthworms at the study sites, i.e., endogeic, epigeic, and anecic. Endogeic and epigeic earthworms that live in mineral soil above soil surfaces mainly form small and tortuous pores ranging between 2 and 5 mm in diameter in size (Pérès, Cluzeau, Curmi, & Hallaire, 1998). Therefore, anecic species form pores size larger than 5 mm in diameter may reach as deep as 2 m into the soil (Edwards & Bohlen, 1996) and subsequently enhance infiltration into deep soil layers (Shuster, Subler, & McCoy, 2002). Different ecological group of earthworm has different impact on water flow also vary with burrowing behaviors through soil. (Edwards, Shipitalo, Owens, & Norton, 1990).
Effect of CEC
CEC showed a positive and highly significant relationship with earthworm’s abundance (p < 0.01). Also, CEC was highest 22.4 ± 1.81 meq/100 in the forest soils of Gajapati district, Odisha India which coincided with the highest earthworm abundance. The CEC is an electrochemical process by which earthworm obtains nutrients. Cation exchange requires very small particles with a large surface area to hold electrically charged ions. This reason may also account for the significant differences in the CEC of the casts compared with three different habitats at various sample collection sites. The exchangeable acidity (cations) was lowest in the agricultural lands of Rayagada and Ganjam districts but these differences were, however, not statistically significant. The species abundantly present in these regions were Lampito mauritii, Octochaetona surensis, and Pontodrilus bermudensis. However, both the positive and negative charges are present on colloid surfaces, and soils of this region dominated. Therefore, more cations (positive ions) attracted to exchange sites than anions (negative ions), and soils seems to have greater cation exchange capacities. Soil pH is one of the crucial soil properties found to be positively correlated with CEC (Foth, 1990). The CEC of soil organic matter and some clay minerals varies with pH. CEC is lowest at soil pH of 3.5 to 4.0 and increase in the pH increased by liming an acid soil most probably. Soil organic concentration also influences pH value of surface soils, since it contributes a significant fraction of soil cation exchange capacity and causes the dissociation of weak acid functional groups on soil organic matter (Brady & Weil, 1996).
Earthworm is one of the important components of soil ecosystem and has a key role in the development and maintenance of physico-chemical properties of soil by converting biodegradable materials and organic wastes into nutrient rich components. In the present study, ten species identified which belong to five different families are as follows: Lampito mauritii, Perionyx excavates, Pontodrilus bermudensis, Perionyx gravely, Eudrilus eugeniae, Octochaetona surensis, Pontoscolex corethrurus, Octochaetona serrata, Pheretima alexandri, and Eisenia fetida. Four species, i.e., Pontodrilus bermudensis, Parionyx excavates, Pheretima alexandri, and Lampito mauritii, are found most abundantly in forest lands, while the other six species are mostly found in agriculture and grass land. The populations of Eudrilus eugeniae, Octochaetona serrata, and Octochaetona surensis are found abundantly in several agricultural lands. Eisenia fetida, Pontoscolex corethrurus, and Perionyx gravely species are mostly found in the areas of grass lands. However, some of the populations are found at both the habitats of forest and grass land such as Lampito mauritii and Parionyx excavates. Principal component analysis also proved that several physico-chemical properties (OC, N, WHC) of soil has found positively influenced the abundance and distribution of earthworms across three land use patterns. In our study, it is noticed that the distribution of earthworm was higher in forest lands and followed by grasslands having high organic manure rather than agricultural land. Therefore, agricultural practices are needed to maintain such a way that confirming the availability of such earthworm population in field for long-term soil productivity.
We are highly thankful to the School of life sciences, Sambalpur University, Odisha for providing laboratory with equipment’s and Zoological survey of India, Kolkata for helping in identifying the species.
This research work was funded by UGC New Delhi.
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