Original articleEffect of biochar addition on soil microbial community in a wheat crop
Introduction
Biochar is produced by low-temperature (400–500 °C) pyrolysis of biomass (such as manure, organic waste, bioenergy crops, crop residues) in oxygen-free or low-oxygen environment. After pyrolysis of the biomass, about 50% of the original biomass C remains in the biochar [1]. Used as a soil amendment, biochar can enhance nutrient availability to plants and improve physical and biological properties of the soil [2], [3], [4], [5], [6]. Moreover, because of its molecular structure dominated by aromatic C blocks, biochar is much more resistant to microbial decomposition than uncharred organic matter [7] and can persist in the soil from 1000 to 10,000 years [8], thus increasing soil C storage [9]. In addition, biochar might improve soil fertility on the long term, mainly by indirect effects, such as increase of cation exchange capacity, surface area and water retention in soil pores, which decreases nutrient leaching, and, to a minor extent, as a consequence of direct nutrient release [2], [10]. The use of biochar has been advocated not only in addressing the widespread problem of loss of soil organic matter and consequent reduction of fertility, but also as a manageable option to dispose of organic waste and favour C sequestration in soil [11].
Beneficial effects of biochar application on crop yield have been documented [12], [13], [14], but specific effects on the soil microbial community are still poorly explored. Yet, soil microorganisms play a central role in nutrient cycling and provide thus an important ecosystem service [15]. Biochar, or at least some labile biochar compounds, has been found to be a potential source of organic matter and inorganic nutrients for microorganisms [16] and can act as a refuge protecting microbes from predators [8]. In fact, biochar pores may be below 5 μm in diameter [17], thereby being accessible to bacteria and fungal hyphae but not their larger predators such as mites and collembolans or most nematodes and protozoans [18], [19]. In addition, biochar can bind toxic compounds such as heavy metals, polycyclic aromatic hydrocarbons and organic pesticides, thus reducing their bioavailability [20], [21], [22], [23], [24]. However, the current information on the effect of biochar on microbial community is not univocal. Organic pyrolytic products, such as phenolics and polyphenolics, may be present in biochar and negatively affect soil microorganisms [25]. Negative, null or positive effects of biochar on soil microbial community have been reported depending on the biochar employed and type of soil [11], [16], [26], [27], [28], [29]. Moreover, only few of these studies have been performed in the field [26], [29], where usually a greater number of factors interacts compared to laboratory conditions. The topic clearly demands further investigation to be performed in the field considering specific biochar, soil and plant cover types. A further aspect that needs consideration is how long the impact of biochar addition, if evidence is provided of positive or negative effects, lasts in time. With the aim to address the above questions, the present study was performed in an agricultural soil in the Mediterranean area, with a focus on microbial quotient (microbial C % organic C), microbial activities, and microbial functional and genetic diversity. These parameters are known to vary in response to several environmental factors including plant cover, land use, agricultural management, pH, salinity, heavy-metal contamination and fire [30], [31], [32], [33], [34], [35], [36], [37], [38], and only rarely have been considered simultaneously in field studies on biochar [29]. Moreover, no data are currently available on the topic for Mediterranean crop soils. This research is a part of a larger study also including biochar effects on crop yield [14] and on greenhouse gas fluxes from soil [39].
Section snippets
Study site and experimental design
The study was set in Pistoia (Tuscany, Italy, lat. 43°56′ N, long. 10°54′ E, 65 m a.s.l.) in a fallow area. The soil had a silty-loam texture and had a bulk density of 1.2 Mg m−3, pH 5.2, 21 g organic C kg−1 soil, 1.2 g N kg−1 soil and cation exchange capacity 18 meq/100 g [14]. The experiment was carried out over two growing seasons (2008/09 and 2009/10) of wheat (durum wheat, Triticum durum L., cultivar Neolatino). Total rainfall and mean air temperature for the growing seasons 2008/09 and
Results
The addition of biochar to soil resulted in a significant increase in pH, with higher values at 3 months after treatment. The treatment did not determine significant variations in total organic C (Corg), extractable organic C (Cext), microbial C (data not shown) and microbial quotient (Cmic % Corg) (Table 1). By contrast, microbial activity, evaluated as mean substrate-induced respiration (mSIR), was significantly higher 3 months after biochar incorporation (B303M, B603M) compared with controls
Discussion
The biochar treatment did not significantly change soil total organic C or extractable organic C. This indicates that, up to 14 months after treatment, biochar addition in the form of particles <1 cm did not significantly contribute to the organic C pool present in fine-earth (<2 mm). Clearly, a longer time than the interval considered in the present study is required for biochar to be fragmented into particles below 2 mm as a consequence of physical, chemical and biological degradation. No
Acknowledgements
Thanks are due to Prof. R. Ligrone for helpful comments to the manuscript.
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