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Discoveries in Agriculture and Food Sciences - Vol. 11, No. 3

Publication Date: June 25, 2023

DOI:10.14738/dafs.113.14605.

Bhattacharya, S. (2023). Organic Matter Decomposition: A View on The Fate of Lignocellulosic Materials. Discoveries in Agriculture

and Food Sciences, 11(3). 22-31.

Services for Science and Education – United Kingdom

Organic Matter Decomposition: A View on The Fate of

Lignocellulosic Materials

Susinjan Bhattacharya

School of Agriculture and Allied Sciences,

The Neotia University, Sarisa, West Bengal, India

ABSTRACT

Organic matter decomposition, a complex process with all the physico-chemical and

biological factors leads to breakdown of organic residues. The prime role in this

process is played by microorganisms with their enzymes. The process is beneficial

not only to generate matters of soil fertility enhancement, but also it can lead to the

products that can add value to soil. Slow and difficult matters to be decomposed like

lingo-cellulosic materials can also be subjected to this decomposition process for

the generation of not only new and beneficial microflora, but also products of value.

The present work discusses here in brief the process of organic matter

decomposition and its importance in rice straw breakdown and lignocellulosic

material decomposition.

Keywords: Decomposition, Factors in decomposition, Microorganisms, Enzymes,

Lignocellulose

INTRODUCTION

Decomposition as a complex process involves physico-chemical and biological factors to

breakdown the raw materials to a usable simpler form of substance and usable as a soil

amendment called as manure. There are two ways for the process of decomposition: aerobic

(in presence of oxygen) and anaerobic (in absence of oxygen). Microorganisms play a bigger

role in decomposition. [Texas A&M Agrilife Extension, 2023; UtahState University, 2023]. The

common subjects for decomposition are waste matters. With regard to the ability of the

substrates to undergo decomposition, the different categories are: easily decomposable,

difficult to decompose, recalcitrant to decompose. Waste, discarded and useless materials

without any value can be either solid, liquid, or mixed in nature. Nonbiodegradable wastes,

mainly are synthetic in nature and are difficult to decompose. The alternate option with

nonbiodegradable wastes is to subject them for recycling preceded by seperation of their

elements [Bhansali, 2021; Lee 2018; Singh, 2021; Tigtag, 2023]. The present work discusses

here in brief the process of organic matter decomposition and its importance in rice straw

breakdown and lignocellulosic material decomposition.

ORGANIC MATTER DECOMPOSITION

The breakdown of organic molecules is an important contributor to the ecosystem respiration

and recycler of energy and nutrients in the ecosystem. The process along with the process of

photosynthesis controls net carbon emission form the ecosystems. The process involves

biochemical transformation in breakdown of complex substrates to the simpler forms [Ravn et

al., 2020; Smith and Smith, 2012]. The dead plant remains in soil or plant litter is mineralized

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Bhattacharya, S. (2023). Organic Matter Decomposition: A View on The Fate of Lignocellulosic Materials. Discoveries in Agriculture and Food Sciences,

11(3). 22-31.

URL: http://dx.doi.org/10.14738/dafs.113.14605

and transformed to organic matter through the activities of soil microorganisms. Conversion of

litter to organic matter involves many steps including the site and soil characteristics. Roots

and Arbuscular Mycorrhizal fungi (AM) fungi are one of the key players in litter decomposition.

These contributes to lignin, melanin and glycoproteins as the prime constituents. Litter

transformation occurs along a gradient from above ground soil to the below ground soil,

wherein aboveground litter is converted to humus [Prescott and Vesterdal, 2021]. Herein, the

rate of decomposition of leaf tissue happens faster than the stem or wood decomposition

[Middleton, 2020]. However, the climate plays a crucial role in litter decomposition [Joly et al.,

2023]. Light is a vital factor in semi-arid ecosystems to lead litter decomposition [Austin and

Vivanco, 2006]. The rate and course of litter decomposition influences biomass, nutrient and

physico-chemical properties of the soil [Kumar et al., 2010].

ROTTING, FERMENTATION AND DECOMPOSITION: DIFFERENCES INVOLVED

Decomposition, a term related to ecology is a process of microbial digestion and destruction of

dead material by the microbial process. Fermentation, a metabolic process and controlled

process of decomposition as well as a microbial process dependent on enzymes varies with in

composition of the involved enzymes to those of decomposition process involved enzymes

[Surstromming, 2023]. In contrast, rotting, a state of decaying is an uncontrolled act of

decomposition [Fermenters kitchen, 2023; Lakna, 2022]. The process of composting involves

decomposition, and fermentation or putrefaction (anaerobic process) is an alternative

suggestive to the process of composting (aerobic process) [Feed Innovation Services, 2013;

Merfield, 2013; Organko, 2022; Chesapeake Bay Foundation, 2023; BioBag International AS,

2023].

FACTORS INVOLVED

Physico-Chemical

Composting, a process is dependent upon different factors, like microbial composition and

succession, particle size and surface area of the particle, moisture content, aeration,

temperature, volume of the material, C:N ratio, pH, etc. [Master Gardener, 2023; Nsimbe et al.,

2018; Meena et al., 2021].

Substrate

Substrate quality depends upon the rate of microbial activity in organic matter decomposition.

Flow of C and N to silt and clay fractions depends on the quality of substrate. The process leads

to increased C and N residence times [Cyle et al., 2016]. Rate of decomposition reduces with

ageing of litter and dead plant, animal residues and other substrates are decomposed till the

point wherein they are no more recognizable and referred to at that stage as soil organic matter.

The process of litter decomposition depends upon the interlinked action of three driving

variables: physico-chemical environment, resource quality and decomposer organisms. [Doe

and Johnson, 2009; Cotrufo et al., 2010]. Furthermore, administration of antibiotic alternatives

in decomposition leads to a change in litter bacterial flora, and elevate the abundance of

beneficial bacteria and reduce pathogen prevalence [Pedroso et al., 2014]. The other important

factor that plays role in decomposition is climate [Joly et al., 2023]. In contrast, soil organic

matter can be protected from decomposition physically and chemically. Additionally, low

temperature and C: N ratio, lesser number of decomposers apart from large scale spatial

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separation brings down the rate of decomposition [Nivethadevi et al., 2021]. Activity of extra- cellular enzymes in organic matter decomposition depends on substrate quantity and

availability. Variation in enzymes is also an important factor here. Substrate affinity of enzymes

varies with the temperature sensitivity for polymer hydrolysis and monomer oxidation

[Myachina and Blagodatskaya, 2015]. In shrub ecosystems, effect of nitrogen addition in litter

decomposition remains neutral due to the effect of low temperature and phosphorus limitation.

Additionally, exogenous nitrogen inhibits lignin degradation but promotes breakdown of

readily decomposed litter components [Zhang et al., 2021].

In a summary, substrate availability and decomposer community limits organic matter

breakdown [Wutzler and Reichstein, 2008]. Oxidation of the carbon compounds provides

energy to the decomposers. Breakdown of organic matter is a crucial requirement for energy

and nutrient cycling in the ecosystem food web as well as contributor to the ecosystem

respiration [Ravn et al., 2020; Middleton, 2020]. With the increase in recalcitrant chemical

components in the litter, decomposability rate of litter decreases, and the decrease in

decomposability or substrate quality is a complex process involving direct chemical changes in

the substrate itself and microbial succession in biochemical reactions. Once, the limit value in

decomposition is reached, the process will be proceeding towards a more stabilized soil organic

matter. Thus, at higher initial nitrogen concentrations, C/N ratio comes down, least amount of

organic matter is left over, indicating a stage of stabilized soil organic matter, low

decomposition rate and lower mass loss [BERG, 2000]. Substrates vary with regard to their ease

of decomposition, and in the scale from very rapid decomposable to slow decomposable,

substrates are: (i) sugars, starches and simple proteins, (ii) crude proteins, (iii) hemicelluloses,

(iv) celluloses, (v) fat, waxes, resins, (vi) lignin [Musa, 2023]. Shrub litter decomposes than the

tree litter [Carnevale and Pablo, 2001] [25]. However, breakdown of organic matter helps in

release of nutrients and functioning of the food web [FAO, 2023]. Additionally, climate

indirectly affects litter decomposition by interacting with plant physiology and plant

resorption, affecting chemical composition of the litter at its formative stages [Suseela, 2019].

Quality and quantity of the litter defines ecosystem functioning which inturn depends on plant

species, forest structures, seasons and climate factors apart from soil drainage [Giweta, 2020;

Schnecker et al., 2019; Krishna and Mohan, 2017; Certini et al., 2015; Kumar et al., 2010].

Biological: Enzymes & Microorganisms

The process of composting involves both aerobic and anaerobic microorganisms [FAO, 2023].

There is also involvement of thermophilic bacteria, fungi and actinomycetes [Joseph, 2019].

Thermophilic bacteria succeed mesophilic bacteria. Actinomycetes plays role in breakdown of

materials like newspaper, bark, and other lingo-cellulosic materials. Apart from actinomycetes,

mould and yeasts also help in breakdown of lingo-cellulosic materials. Additionally, protozoa

consume inactive bacteria, fungi and actinomycetes. There are other physical decomposers also

which feed on the organic waste [Editors, 2022]. Furthermore, there are different kinds of

enzymes, like cellulases, hemicellulases, ligininase, chitinases and esterases, etc. with varied

activities that play a role in composting [Finore et al., 2023; Nakamura et al., 2004; Murugesan

and Amarnath, 2020; Infinita Biotech]. Lignin modifying enzymes from different producers acts

at the compost maturity stage [Robledo-Mahon, 2020]. These activities lead to a change in

concentrations of minerals in compost [Bohacz, 2019]. The mesophilic stage also has the

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Bhattacharya, S. (2023). Organic Matter Decomposition: A View on The Fate of Lignocellulosic Materials. Discoveries in Agriculture and Food Sciences,

11(3). 22-31.

URL: http://dx.doi.org/10.14738/dafs.113.14605

presence of bacteroides and proteobacteria as the dominant flora apart from the presence of

bacteria, fungi, etc. [Biyada et al., 2021; Li et al., 2019; Rath et al., 2022].

BREAKDOWN OF LIGNOCELLULOSIC MATERIALS

Lignocellulose, component of a waste biomass breaks down when acted upon by the

lignocellulose-degrading enzymes; cellulases, hemicellulases, laccases and ligninases [Chandra

and Madakka, 2019]. Lignocellulosic material consists of cellulose, hemicellulose and lignin,

wherein cellulose is a homopolymer of glucose residues, and lignin is a complex polymer of

phenylpropane [Sahay, 2022]. The main source of lignocellulosic materials is plant biomass,

and apart from fungi as the primary degraders, bacteria also play an important role as the

potential degraders [deSouza, 2013; Wilhelm et al., 2019]. Lignocelluloses also act as a matrix

wherein enzymatic hydrolysis for biofuel production occurs [Baig, 2020]. Microbial synergistic

consortia of a thermophilic filamentous fungus and thermophilic actinobacterium has been

reported to act as lignocelluose degraders [Shi et al., 2020]. Pretreatment of lignocellulosic

materials also plays role in generation of fermentable sugars [Kucharska et al., 2018]. The best

degraders of lignin in nature are the basidiomycetes white-rot fungi, followed by the brown rot

fungi. Enzymes that play role in the lignin breakdown are namely, laccases, manganese- dependent peroxidases (MnP), lignin peroxidases (LiP), and versatile peroxidases (VP) [Andlar

et al., 2018]. A complex bacterial consortium with species of Actinobacteria, Proteobacteria,

bacilli, Sphingobacteria, and Flavobacteria in an enrichment culture system has been seen to

breakdown different forms of lignocellulose [Georgiadou et al., 2021]. Furthermore, soil

invertebrates also play a role in lignocellulose breakdown [Bredon et al., 2018]. The complex

structure of lignocellulose needs participation and interaction of a variety of microorganisms.

This also highlights upon the importance of conducting more research to elucidate the

collaborative degradation mechanisms [Zhu et al., 2021].

BENEFITS OF ORGANIC MATTER DECOMPOSITION

Organic matter decomposition leads not only to the formation of humus, but also provides

compost that improves soil structure, add plant nutrients and beneficial microorganisms to the

soil. Addition of antibiotic, or antibiotic alternative helps to enrich beneficial microbes in the

litter and compost [Pedroso et al., 2014]. Long term administration of compost to soil helps in

improving the soil structure. Rice straw rich in ligno-cellulose when subjected to composting

improves not only the microbial diversity, but also the grain yield and grain quality [Huang et

al., 2023]. Paddy straw when left over in the field can neither be used as food or feed, but can

be composted to generate a compost of better quality as well as return back of nutrients to the

field [Nghi et al., 2020; Singh et al., 1995]. This helps also in generation of effective

lignocellulose degraders [Goyal and Sindhu, 2011; Shruti et al., 2015]. Lignocellulosic biomass

upon degradation leads also to the generation of high value products [Cecilia et al., 2021].

CONCLUSION

Organic matter decomposition involves the stages of: photo-oxidation, leaching, comminution

and mineralization and depends on a number of interacting processes [Schowalter, 2016;

Wantzen et al., 2008]. Composting is a process that speeds up the natural process of

decomposition in presence of microorganisms [Albright and Martiny, 2018]. Paddy straw

composting not only increases microbial activity and rate of composting but also improves the

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degrading microflora [Jusoh et al., 2013, Nghi et al., 2020; Huang et al., 2023]. Enrichment of

the process with cellulolytic bacteria in paddy cultivation led to an improved and better rice

yield [Lestari et al., 2020]. The process of organic matter decomposition is understood

experimentally from the view point of composting and humus formation. Thus, composting as

a process highlights also upon the discovery of more efficient lignocellulose degraders, apart

from helping to improve the soil quality and enrich the soil with beneficial nutrients and

microflora.

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