Physico-chemical characteristics of soils
Physicochemical characteristics of
Medicogo sativa,
Medicago truncatula and
Trifolium rubens rhizospheric soil samples were studied (Table 2).
Particle size characterizations indicated that different soils showed a sandy texture (more than 82%) with very little clay (3.33-5.33%) and silt (9-12%). The three soils samples displayed an alkaline pH with values varying from 8.42 to 8.49 (Table 2). The studied soils expressed total limestone contents ranging from 7 to 12%. The highest content (11.58%) corresponded to
Medicogo sativa, followed by
Trifolium rubens (9.38%) and
Medicago truncatula (7.73%) (Table 2).
Soil organic matter is made up of living and decaying organisms such as plants, animals and microorganisms. It represents generally 0.5 to 10% of the soil. The rhizospheric soils of the species
Medicago truncatula,
Medicago sativa and
Trifolium rubens organic matter contents were 5.71%, 8.03% and 9.52%, respectively. Carbon and nitrogen are a major product of various organic compounds, such as bacteria and fungi decaying organisms, mineralization. Interestingly,
Medicogo sativa rhizospheric soil carbone content was higher (5.54%), compared to
Trifolium rubens (4.67%) and
Medicago truncatula (3.32%). However, soil with the lowest carbon content (
Medicago truncatula) displayed the highest nitrogen rate (0.36%) and the other soils contained less nitrogen (0.18-0.2%) (Table 2). Phosphorus is one of the major elements essential for the growth and development of plants. It plays an critical role in the establishment of the root system, photosynthesis and plant reproduction. Studied soils phosphorus contents were similar for
Medicago sativa and
Trifolium rubens and higher (0.98 ppm) for
Medicago truncatula soil (Table 2).
Soil cationic exchange capacity represents the reservoir size enabling the reversible storage of certain cationic fertilizing elements such as potassium, magnesium and calcium.These cations can be weak acids or strong acids, depending on the pH. For the three rhizospheric soils, calcium (Ca) content was greater than 20 mg/l, potassium (K) between 18 and 22 mg/l, magnesium (Mg) between 24 and 31 mg/l and natrium (Na) varies from 10 to 12 mg/l (Table 2).
Medicago trucatula significantly improves soil tenure in terms of total carbon, organic matter, total nitrogen and available phosphoore compared to
Medicago sativa and
Trifolium rubens.
Soil physicochemical characteristics were plant depending suggesting
Medicogo sativa,
Medicago trucatula and
Trifolium rubens growth influence on soil parameters. Likewise, changes in the edaphic parameters were observed following a symbiotic associations plant-microorganisms
(Hodge et al., 2001; Chen et al., 2018).
Our results agreed with
Baize and Jabiol (1995) pedological reference, indicating that the plant species
Medicogo sativa,
Medicago trucatula and
Trifolium rubens rhizospheric soils had an alkaline pH. This parameter is one of the most important indicators of soil quality
(Liu et al., 2006). In arid and semi-arid environments like that of the region of our study (the Chlef ecosystem, Algeria), pH can be strongly influenced by climate and vegetation
(Smith et al., 2000). It increase is mainly due to low leaching given the low rainfall characterizing these regions
(Wezel et al., 2000). The studied plants were growing in a sandy soil. Such a sandy texture is the sign of a well aerated soil while too much clay is indicative of an impermeable and poorly ventilated environment, thus forming an obstacle to the penetration of roots. The texture greatly influences the chemical composition of sandy soils (
Koske and Halvorson, 1981). These soils are generally poor in nitrogen and available phosphorus (
Brundrett, 1991). mycorrhizal plants can however improve soil fertility
(Fall et al., 2022).
Soil organic matter content is usually influenced by climatic factors, vegetation, soil texture, topographic conditions, drainage and cultivation practices (
Drouet, 2010). Studies legumes’ soils can be considered as very rich in organic matter with contents higher than 5.7%. The richness of the soil in organic matter is increased by the renewal of roots and leaves and by litter decomposition in addition to organic nitrogen decomposition enhanced by arbuscular mycorrhizal fungi (
Hamel and Plenchette, 2017).
Mycorrhizal infectious potential (MIP)
The MIP50, is non-sterilized soil quantity of required to mycorrhize 50% of plants, varied among the three soils.
Medicago truncatula significantly improved soil MIP50 with a value of (23.80) compared to
Trifolium rubens and
Medicago sativa which had (21.75) (20.28) respectively (Table 3).
Terrestrial microbial biodiversity is recognized as a potential biofertilizer with the capacity to enhance soil fertility and support plant performance under environmental stresses (
Gentili and Jumpponen, 2006). Mycorrhizal fungi, in particular, are regarded as vital biological agents for soil restoration, promoting plant growth, aiding in water and mineral nutrient uptake and contributing to plant protection
(Duponnois et al., 2005; Cardoso and Kuyper, 2006).
Plants with a high mycorrhizal dependency play a pivotal role in fostering fungal proliferation, consequently elevating the mycorrhizal infectious potential of the soil
(Sellal et al., 2021). Leguminous plants are generally classified as hyper-mycotrophic species capable of stimulating the multiplication of fungal symbionts and enhancing the MIP of the soil
(Duponnois et al., 2013).
Root colonization
Microscopic observation of mycorrhizal forms
The roots of
Medicogo sativa,
Medicago atrucatula and
Trifolium rubens underwent treatment following the procedure outlined by
Phillips and Hayman (1970). Microscopic examinations unveiled the presence of diverse endomycorrhizal structures, including hyphae, vesicles and arbuscules (Fig 1).
Estimation of mycorrhization rates
The frequency of mycorrhization exceeded 90% in these plants, indicating their suitability as valuable mycorrhizal inoculum material or nurse plants. Furthermore, the cortex colonization intensity and mycorrhization intensity of the mycorrhizal fragments exceeded 70% for all plant species. The arbuscular percentage of the mycorrhizal fragments also exceeded 50% (Fig 2).
According to
Read (1989), sandy soils are known to host diverse arbuscular mycorrhizal fungi and a rich, varied and ecologically beneficial microflora (bacteria and fungi)
(Hu et al., 2010). The presence of arbuscules, considered the primary site of nutrient exchange, signifies that plants have established functional symbiosis
(Mishra et al., 2018). Moreover, plant colonization is contingent upon the affinity between plant and fungi species, which can influence the abundance and composition of mycorrhizal fungi
(Lovelock et al., 2003). Several experimental studies have shown that soil characteristics influence the diversity and community composition of AMF colonizing plant roots in various sites or habitats
(Alguacil et al., 2016; Casazza et al., 2017; Sarkodee-Addo et al., 2020).
Principal component analysis (PCA)
Projection onto the factorial plane (F1 × F2) of data corresponding to the two factors: physicochemical and microbiological characteristics, respectively, for the diverse soils associated with the plant species has been given in Fig 3.
The utilization of Principal Component Analysis (PCA) enabled the graphical representation of the interrelationships among various physicochemical parameters and the Mycorrhizal Infectious Potential (MIP50) of the soils under investigation. The two principal axes account for a cumulative variance of 70.56% in total.
The first axis regroups parameters such as available phosphorus, total nitrogen, conductivity, pH and MIP50, which were positively correlated with ranging from 0.86 to 0.89. This axis accounts for the largest proportion of variance (43.27%). Conversely, negative correlations were observed between carbon and both phosphorus and MIP50, with correlation coefficients of -0.72 and -0.91, respectively.
The second axis, responsible for 27.30% of the variance, exhibits a positive correlation between nitrogen and available phosphorus, with a correlation coefficient of 0.84.
MIP50 corresponds to the amount of unsterilized soil (which contains mycorrhizal microorganisms) needed to mycorrhize 50% of plants, which explains the correlation of PIM50 with nitrogen and phosphorus, mycorrhizal symbiosis improves the amount of these two elements in the soil (
Vanek and Lehmann, 2014;
Dejana el al., 2022).
He et al., (2021) found that
Medicago sativa improves significantly the nitrogen and phosphorus amount in soil rich in mycorrhizal propagules and rhizobia.