Open access peer-reviewed chapter

Enhancing Agriculture through Strategic Tillage and Soil Management: Unleashing Potential for Sustainable Farming

Written By

Mahima Dixit, Debabrata Ghoshal, Sanjeev Kumar and Debashis Dutta

Submitted: 25 July 2023 Reviewed: 28 August 2023 Published: 19 June 2024

DOI: 10.5772/intechopen.113038

From the Edited Volume

Strategic Tillage and Soil Management - New Perspectives

Edited by Rodrigo Nogueira de Sousa

Chapter metrics overview

29 Chapter Downloads

View Full Metrics

Abstract

Modern agriculture relies on strategic tillage and soil management to improve soil health, crop yield, and environmental impact. Innovative tillage methods reduce soil disturbance and use alternative soil management methods. Poor tillage reduces soil health and productivity. Some of them include soil erosion, runoff losses, compaction, organic matter deuteration, and nutrient losses. For long-term environmental sustainability, it is important to recognize the risks of improper tillage and implement sustainable soil management methods that reduce soil disturbances, conserve organic matter, improve soil structure, and promote soil stability. In the modern day, mechanization and industrialisation have greatly impacted soil health and ecological balance. This chapter provides a brief review of strategic tillage and soil management concepts, benefits, and challenges. It highlights the shift from traditional tillage to balanced soil management strategies. Strategic tillage improves soil health, conserves resources, decreases erosion, and ensures agricultural resilience and sustainability by limiting soil disturbance, retaining organic matter, and improving fertilizer management. The chapter also highlights aspects cover crops, precision agriculture, and organic farming for soil quality and resource efficiency. This chapter begins to explore the importance and implications of strategic tillage and soil management in modern agriculture.

Keywords

  • soil management
  • tillage
  • sustainability
  • crop productivity
  • climate change

1. Introduction

Globally, the agricultural, farming sectors and environmental sustainability are inherently reliant on each other. However, they have undergone significant transformations by mechanization of agriculture, which includes advancements in technology, expansion of operations, socioeconomic progress, alterations in consumption habits, and the looming ignorance of environmental deterioration. About half of Earth’s arable land is now used for farming, ranching, or grazing. However, farmers and land managers have altered agricultural ecosystems through resource extraction and wasteful use, in an effort to boost food production for local consumption and export. According to statistics, approximately 2.37 billion individuals, accounting for nearly one-third of the global population, in the 2020 had insufficient access to food due to a lack of resources [1]. Consequently, the challenges of food and nutrition insecurity, in conjunction with climate change, have emerged as the foremost critical and pressing concerns in the pursuit of the Sustainable Development Goals and the goals that are delineated in Agenda 2063.Currently, nations across the globe, both developed and developing, are confronted with pressing and interrelated challenges. These challenges pertain to the critical issues of ensuring food security for a rapidly growing population, as well as the restoration of the environment and preservation of natural resources. In an era marked by population growth, climate change, and escalating environmental concerns, the quest for sustainable agricultural practices has become imperative. At the heart of this endeavor lies scientific tillage, a crucial approach to land cultivation that strives to strike a harmonious balance between agricultural productivity and ecological preservation. Unlike traditional, indiscriminate tillage methods, scientific tillage is an evidence-based, technologically driven approach that recognizes the profound impact of human activities on the planet. By harnessing cutting-edge research and innovative techniques, scientific tillage plays a pivotal role in maintaining sustainability in agriculture, safeguarding soil health, mitigating environmental degradation, and securing the future of food production for generations to come. Consistent use of conventional tillage has been shown to degrade soil structural stability, soil biological characteristics, and nutrient storage and supply, according to growing experimental evidence [2, 3]. After the harvest of Rabi and Kharif season crops, conventional tillage entails a series of mechanical procedures to prepare the soil for the next planting season. These operations include deep plowing, deep disking, ripping, shallow-type workings, and fine seedbed preparation. Subsequently, a designated period of fallow is implemented to facilitate the capture of moisture prior to the commencement of planting the subsequent crop. This method leads to the exposure of a bare soil surface, making it susceptible to erosion caused by wind and water. Additionally, heavy rainfall can result in high compaction, necessitating the need to loosen the soil again for weed control and to enhance moisture absorption during subsequent rain events. Tillage strategies change soil physicochemical characteristics, consequently modifying crop yields [4]. The ongoing degradation of soil in arable land, caused by improper tillage practices, has a notable impact on the physical, chemical, and biological properties of the soil. This leads to a reduction in the storage of soil organic carbon (SOC), as well as a decline in crop productivity and the value of ecosystem services within agricultural systems [5]. There is a prevailing belief that the primary factor contributing to the historical depletion of soil organic carbon (SOC) in North America is soil disturbance caused by tillage. It is widely acknowledged that a significant increase in SOC sequestration can be achieved by transitioning from conventional plowing to less intensive techniques commonly referred to as conservation tillage. Soil tillage modifications bring in a change in soil structure, and therefore, a strategic method of tilling the soil according to the soil type, structure, and environmental condition can prove an effective method to combat carbon losses and other land degradation happening [6]. The soil health plays a vital role in the managing critical zone of the Earth. To effectively work toward the attainment of the United Nations’ Sustainable Development Goals (SDGs), it is imperative to uphold fundamental ecosystem services such as food production, plant growth, animal habitat, environmental preservation, carbon sequestration, and overall environmental sustainability. Soil degradation has been observed in various locations worldwide as a result of faulty agricultural practices and lack of knowledge about the new technologies. To effectively accomplish the Sustainable Development Goals (SDGs) within the designated timeframe of 2030, it may be necessary to adopt and implement more sustainable approaches to the utilization and management of soils, surpassing current practices. In this study, we demonstrate the importance of prioritizing the arena of sustainable soil use and management. Specifically, we emphasize the need to focus on the multifunctional tillage practices and their interdisciplinary linkages with major issues concerned with soil health and environment sustainability.

Advertisement

2. Tillage systems

Tillage systems refer to various methods and practices used in agriculture for preparing the soil for planting, managing crop residues, and controlling weeds. These systems involve different degrees of soil disturbance and manipulation to create an optimal environment for crop growth and maximize agricultural productivity. Soil organisms’ natural habitats are strongly influenced by the tillage technique used because of the profound effects that system has on the soil’s physical and chemical environment. Tillage techniques can affect the soil’s moisture, temperature, airflow, and degree of crop residue integration. The changes in soil physical conditions have both direct and indirect impacts on the climate and ecosystem dynamics (Figure 1). A significant challenge in the field of soil ecology research involves comprehending the effects of management practices on the intricate interactions among various organisms within the soil community. Soil manipulations alter the living community of soil in several ways. The microorganisms in soil play a crucial role by performing essential functions such as enhancing soil structure, facilitating nutrient cycling, and facilitating degrading of organic matter [8]. The fundamental motivation for reducing tillage intensity and to shift toward innovative methods is to lessen the financial burden of tillage in the context of commercial agriculture and to reduce the amount of soil degradation sometimes associated with excessive tillage techniques as well as the indigenous techniques of tillage that cause major problems in the soil–environment dynamics as compared to the innovative techniques (Table 1). Tillage needs vary moderately according to the crop and soil type. It may not always be necessary or desirable to till an entire field at once. Row crops including corn (Zea mays L.), sugar beets (Beta vulgaris L.), and oilseed rape (Brassica napus L.) can have their tillage restricted to certain areas of the field, a method known as strip or zone tillage. The process of seedbed preparation can be limited to the specific area where the seeds will be planted, while the rest of the land may undergo a reduced or alternative form of tillage. In the non-planted regions, a soil structure with a coarse texture is deliberately maintained to enhance the process of water infiltration. In addition to the aforementioned, crop residues might be left on the soil’s surface in the spaces between rows of plants. This method is used to reduce water loss due to evaporation and to protect the soil from wind and precipitation.

Figure 1.

Tillage systems as an interwoven element in managing the agroecosystems [7].

AspectTraditional tillage methodsNew innovative tillage techniques
Soil DisturbanceExtensive soil disturbance using plows and heavy equipmentMinimal to no soil disturbance to preserve soil structure and reduce erosion
Crop Residue ManagementCrop residues are often buried or removedCrop residues are left on the surface to improve soil health and moisture retention
Weed ControlGood initial weed control due to soil disruptionMay require additional weed management strategies, but can benefit from reduced competition over time
Soil ErosionCan lead to increased soil erosionReduced erosion due to better soil structure and residue cover
Organic Matter ContentMay result in a decrease in organic matter over timeHelps build and maintain organic matter content in the soil
Soil AerationProvides initial soil aerationMay improve soil aeration over time due to increased soil health
Water ConservationLess effective in conserving waterBetter water conservation due to reduced soil disturbance and residue cover
Energy and Labor RequirementsCan be labor- and energy-intensiveOften reduces the need for intensive tillage equipment, leading to lower energy and labor requirements
Soil Health and BiodiversityMay negatively impact soil health and biodiversitySupports soil health and promotes biodiversity due to reduced disturbance and increased organic matter
Adaptability and ChallengesWell-established and widely used, but can be environmentally challengingMay require adaptation in weed and pest management, but promotes long-term sustainability

Table 1.

A comparison between the traditional tillage practices and the innovative tillage practices, the challenges, and the constraints.

The fundamental soil tillage operations encompass either soil inversion or fragmentation. Various tillage implements are employed to carry out tillage operations, operating at specific soil depths. The process of soil inversion is most effectively executed through the utilization of a moldboard plow, whereas soil loosening can be accomplished by employing various tillage tools. Rotary cultivators are highly suitable for the purpose of soil mixing, frequently employed for the integration of soil fertilizer and organic amendments into the soil. The presence of plant residues has the potential to impede the functionality of certain tillage implements. In agricultural practices, coulters or disks are frequently employed to effectively sever or redirect crop residue from the immediate tillage zone. The occurrence of frequent or intense vehicular movement within the agricultural area can result in the compaction of the subsoil, which refers to the soil located beneath the depth at which tillage activities are performed. Subsoiling refers to the application of mechanical techniques aimed at loosening the compacted subsoil, as outlined in remedial tillage operations. To ensure optimal results, it is recommended that the subsoiling operation be conducted when the soil exhibits a friable consistency, thereby minimizing the risk of smearing. A subsoil that has been mechanically loosened exhibits a diminished strength and is susceptible to significant recompaction with relative ease.

Advertisement

3. Soil and tillage

The composition of soil consists of both living and nonliving components that are arranged in a vertical profile, characterized by horizontal layers or horizons. Soil serves as the habitat for a wide variety of living organisms, encompassing a multitude of microscopic species such as bacteria, fungi, protozoa, nematodes, and microarthropods [9]. Mechanically altering the soil’s physical condition in order to improve plant growth for human and animal food production is known as tillage. Plant nutrients and crop additives can be worked into the soil during tillage operations including bed preparation, planting, and postemergence cultivation for weed control. Tillage needs change from crop to crop, depending on things like soil composition and weather. Damages to the environment and agricultural production systems may result if the intensity of tillage is not enough for the local conditions [10]. The fundamental soil tillage operations encompass soil inversion or fragmentation, as outlined in Table 1. Various tillage tools are utilized to perform these operations, operating at specific soil depths. The process of soil inversion is most effectively executed through the utilization of a moldboard plow, whereas soil loosening can be accomplished by employing various tillage tools. Rotary cultivators are highly suitable for the purpose of soil mixing, commonly employed to incorporate soil fertilizer and organic amendments into the soil. Plant residues have the potential to impede the functionality of certain tillage implements. Coulter blades or disks are frequently employed to effectively sever or redirect crop residue from the immediate tillage area. Frequent or excessive traffic in the field can result in soil compaction in the subsoil, which refers to the soil located beneath the tillage depth. Subsoiling refers to the application of mechanical techniques to alleviate compaction in the subsoil layer (Figure 1, Table 1). For optimal subsoiling, it is recommended to conduct the operation when the soil has a water content that allows for friability, thus preventing smearing. A subsoil that has been mechanically loosened exhibits diminished strength and is susceptible to significant recompaction (Figure 2).

Figure 2.

A pictorial representation of the various tillage operations that provides an overview of the advantages and disadvantages of soil tillage and the various operations in cultivating soil using conventional, reduced and no-till tillage systems, particularly in relation to plowing [11].

Advertisement

4. What is strategic tillage?

Strategic tillage is an agricultural practice that involves the targeted and deliberate use of tillage operations in specific areas and at specific times to achieve specific goals. Tillage refers to the mechanical manipulation of the soil through plowing, digging, or turning it over. The concept of strategic tillage recognizes that excessive or indiscriminate tillage can have negative effects on soil health, such as soil erosion, loss of organic matter, and disruption of soil structure. Therefore, strategic tillage aims to optimize tillage operations to minimize these negative impacts while maximizing the benefits for crop production [12].

Advertisement

5. Historical background and evolution of strategic tillage practices

The historical development of strategic tillage practices can be categorized into distinct stages. Early agricultural practices involved manual methods such as hand digging, which gradually evolved with the introduction of animal-drawn implements, including the plow. The Industrial Revolution spurred mechanization, leading to increased tillage efficiency but also raising concerns about soil degradation. The emergence of conservation tillage in the mid-20th century marked a significant transition toward sustainable land management, highlighting the need for minimizing soil disturbance and preserving soil health. However, it was the integration of advanced technologies and ecological insights that paved the way for modern strategic tillage practices. The incorporation of precision agriculture tools, remote sensing, and geospatial data analysis enabled farmers to target tillage operations based on field variability, optimizing resource use and minimizing environmental impacts. The adoption of strategic tillage practices aligned with the principles of conservation agriculture, involving reduced tillage, conservation tillage, and minimum tillage and emphasizing soil conservation, nutrient management, and ecosystem resilience.

Advertisement

6. Strategies for implementing strategic tillage for soil management

6.1 Conservation tillage

The phrase “conservation tillage” can be used to describe a wide variety of approaches to soil management. As per the research conducted by Mannering and Fenster in 1983 [13], conservation tillage can be defined as a tillage system that aims to minimize soil or water loss in comparison to conventional tillage practices. This frequently entails the utilization of non-inversion tillage techniques that maintain an adequate layer of residue mulch on the surface of the soil. As per the CTIC, conservation tillage is a designated tillage and planting approach that guarantees a minimum of 30% soil surface coverage through residue after planting. Table 2 describes the various aspects of conservation tillage. The primary objective of this system is to effectively mitigate water and wind erosion and conservation of soil. In order to keep soil losses to a minimal, it is imperative that certain standards be upheld while taking into account the wind and water conditions. Alternative conservation tillage methods focus on keeping at least 1000 pounds of flat, tiny grain residue equivalent on the soil’s surface throughout the critical wind erosion period. Conservation tillage can be broadly mechanized into the following categories that hold a significant difference in soil management.

No tillageRidge tillageMulch tillageConventional tillage
This method relies on herbicides, cover crops, or both to keep weeds at bay and requires relatively little mechanical seedbed preparation (a narrow band where the seed is sown).Sweeps, disk openers, coulters, or row cleaners are used to prepare ridges in the seedbed before planting. Between the ridges, the residue is left behind. Herbicides and horticulture are both effective methods for eradicating weeds (CTIC*).The soil is disturbed prior to plantingGenerally, it refers to moldboard plowing (inversion of the soil) followed by a secondary tillage operation such as disking and/or harrowing
With the exception of potential fertilizer injection, no-tillage methods involve not disturbing the soil between harvesting and planting.From harvest to planting, only fertilizer injections are made to the soil.Chisels, field cultivators, disks, sweeps, and blades are all examples of tillage implements. Herbicide and/or cultivation are used for weed management.Both cultivation and the application of herbicides are viable options for weed management.

Table 2.

A comparison between the various tillage systems under conservation tillage.

The Conservation Technology Information Centre (CTIC).


6.2 Reduced tillage

Targeted and suitable tillage that takes into account the specific needs of the farm is at the center of reduced tillage methods. With reduced tillage, the depth and width of the bed, field, and overall farm are all worked on with a lesser intensity. Due to their beneficial effects on soil and water conservation [14, 15] and their ability to lower the demand for fuel, equipment, and labor [16], the use of reduced tillage practices is on the rise worldwide [17]. Due to the reduced level of soil disturbance associated with reduced tillage as compared to conventional tillage, there is a limited mixing of plant residues, fertilizers, and other soil amendments into the soil. Consequently, plant roots have a tendency to proliferate primarily in the uppermost few centimeters of the soil. In addition, the uppermost layer typically exhibits higher moisture levels, lower temperatures, reduced oxidation, and increased acidity [18, 19, 20]. Under these conditions, it is observed that the organic matter content tends to exhibit a slower rate of increase or decrease in comparison to that under conventional tillage practices. In addition, the adoption of straw mulching and reduced tillage practices has a significant influence on the microenvironment of soil microorganisms, consequently affecting the overall sustainability of the environment [21].

6.3 Zero tillage

When referring to a tillage system, the term “zero tillage” is used to indicate that only traffic and seedbed preparation are performed mechanically on the soil. It is the most extreme kind of minimum tillage, a grouping of tillage systems that includes the plow–plant method and other practices that decrease the amount of soil disturbed during cultivation. Compared to conventional tillage (CT), zero tilling (ZT) causes immediate and substantial alterations to the soil pore network. Long periods of time without disturbing the soil allow biotic and abiotic processes to work together to create a stable soil structure [22]. Plant matter is allowed to remain on the soil’s surface under a zero-till system. This is crucial in cases where soil erosion prevents farming from being profitable. The observed proportionate increase in the number of medium to tiny pores generated by zero tillage has implications for the soil’s water-holding capacity. The act of plowing grassland results in the redistribution of organic matter, whereas zero-tilled sod retains its original deposit of organic matter in close proximity to the soil surface. Baeumer and Bakermans [23] discovered that water content at pF 2 changed more in association with organic matter content than with soil porosity. As a result, the top 6 cm of the zero-tilled soil had a larger water content at pF 2 than that of the plowed soil.

6.4 Minimum tillage

The minimum tillage approach is a soil conservation system that shares similarities with strip-till. Its primary objective is to minimize soil manipulation while still achieving successful crop production. No-till farming is a cultivation technique that avoids soil inversion, as opposed to intensive tillage practices that involve the use of plows to alter the soil structure. In the practice of minimum tillage, primary tillage is entirely omitted, and only a limited amount of secondary tillage is employed. The practice of minimum tillage encompasses various techniques, such as minimizing furrowing, employing organic fertilizers, utilizing biological pest control methods, and reducing reliance on chemical inputs. The application of minimum tillage (MT) in combination with organic farming has proven to be effective in promoting the improvement of the biomass of soil microbe. The microbial community structure experiences a shift toward bacteria within organic farming systems. Bacterial populations demonstrate a more prominent reaction to agricultural practices in comparison to other groups of microorganisms. This response is particularly evident when minimum tillage techniques are employed, as they contribute to the improvement of soil’s biological properties. Consequently, these practices indirectly influence the overall health of the soil [24].

Advertisement

7. Conventional vs. conservation: benefits of conservation tillage on soil properties

7.1 Soil physical properties

The impact of conservation tillage on soil physical properties can vary depending on several factors, including soil type, climate, prevalent cropping system, and managerial practices. Nevertheless, conservation tillage, on the whole, facilitates the enhancement of soil integrity, control of erosion, infiltration of water, conservation of moisture and organic matter content, and the reduction of soil compaction, thereby resulting in improved soil physical properties. The effects of conservation tillage on soil properties demonstrate variability, with the choice of a specific system playing a pivotal role in determining these variations. No-till (NT) systems, characterized by the maintenance of extensive surface soil coverage, have been found to induce notable alterations in soil properties, particularly within the upper few centimeters [25]. Numerous studies have indicated that the utilization of NT (no till) has led to a significant enhancement in both saturated and unsaturated hydraulic conductivity. This improvement can be attributed to either the preservation of pore continuity, as observed by Benjamin in 1993 [26], or the facilitation of water flow through a limited number of larger pores. According to Butorac [27], there is evidence indicating that soils with good drainage, a light to medium texture, and low humus content demonstrate an optimal response when exposed to conservation tillage practices, specifically no tillage. According to the research conducted by Lal et al. [28], it has been established that the adoption of NT technologies offers notable advantages in terms of mitigating soil and crop residue disturbance, regulating soil evaporation, and reducing erosion losses. It has been observed that no-till (NT) soils exhibit a greater presence of stable aggregates in the upper soil surface when compared to in tilled soils. As a result, this leads to an increased overall porosity in the NT plots. According to a study conducted by Pagliai et al. [29], minimum tillage was found to enhance the soil pore system when compared to conventional plowing. The observed improvements were characterized by an increase in the storage pores ranging from 0.5 to 50 mm, as well as an increase in the quantity of elongated transmission pores ranging from 50 to 500 mm. The researchers established a correlation between the elevated microporosity observed in minimum tillage soils and an associated rise in soil water content. Consequently, this leads to an increase in enhanced water availability for plant uptake. In a study conducted by McVay et al. [30], it was seen that the topsoil (0–10 cm) under no-till (NT) practices exhibited a greater water-holding capacity or moisture content compared to soil that had undergone plowing. Consequently, in order to enhance soil water retention and optimize water utilization efficiency (WUE), numerous scholars have suggested substituting conventional tillage practices with conservation tillage methods [31, 32].

Advertisement

8. Soil chemical properties

The examination of the enduring effects of conservation tillage on soil chemical properties is a subject of considerable importance to farmers, agronomists, and environmentalists. The implementation of conservation tillage practices leads to the creation of a unique soil environment, which in turn requires modified management approaches when compared to conventional tillage methods. Soil pH, cation exchange capacity (CEC), exchangeable cation levels, and total nitrogen content are among the many of the chemical parameters typically affected by the tillage techniques. Lal [33] found that distinct positive changes in chemical properties of the surface layer tend to occur when employing the no-till method compared to tilled soil. Research by Rasmussen [34] shows that plant residues on the soil’s surface contribute to an increase in organic matter inside the topsoil when no-tillage methods are used on a yearly basis. Ismail et al. [35] also documented a notable increase in soil organic carbon (SOC) levels in no-till (NT) soil when compared to in untilled soil. It has been observed that the total nitrogen loss is reduced under the no-till (NT) practice in comparison to under conventional tillage (CT). In tilled lands, the organic carbon and total nitrogen shows a crisp decrease as compared to in land with minimum tillage, which can be attributed to higher rates of mineralization and/or leaching due to the deterioration of soil structure caused by tillage practices; the soil remains unaltered Dalal [36]. The nutrient availability is effectively maintained as the organic matter content is increased in conservation tillage practices. The implementation of conservation tillage practices has been found to have a beneficial effect on the nutrient content of soil. Soils managed with conservation tillage exhibit elevated levels of essential nutrients, including nitrogen (N), phosphorus (P), and potassium (K). The levels of exchangeable calcium (Ca), magnesium (Mg), and potassium (K) in the surface soil are notably elevated under no-till (NT) practices in comparison to under the plowed soil. Conservation tillage systems contribute to the enhancement of nutrient availability for crops by promoting improved soil organic matter content and reducing erosion.

Advertisement

9. Soil biological properties

Conservation tillage practices bring significant changes to soil biological properties compared to conventionally plowed soils. With minimal soil disturbance and increased crop residues left on the soil surface, conservation tillage creates a more favorable environment for soil organisms. One notable impact is the increase in microbial diversity and activity. The continuous supply of organic matter from crop residues fosters microbial growth, leading to enhanced nutrient cycling and improved decomposition of organic materials. This, in turn, boosts nutrient availability for plants, supporting healthier crop growth. Another notable change is the promotion of earthworm and macroinvertebrate activity. The presence of crop residues provides these soil organisms with a constant food source and shelter, leading to higher populations and increased soil bioturbation. The significance of earthworms and macroinvertebrates in the context of soil aeration, organic matter breakdown, and nutrient cycling cannot be overstated. These organisms are instrumental in enhancing soil structure and promoting nutrient availability. The implementation of conservation tillage practices has been found to have a positive impact on the accumulation of soil organic matter. The reduced soil disturbance and slower decomposition rates in conservation tillage systems allow organic matter to build up over time. This accumulation enhances soil biological activity and nutrient retention, promoting a more vibrant and resilient soil ecosystem. Organic carbon is a crucial component that serves as a significant energy source and effectively governs microbial activity within soil [37]. The utilization of conventional tillage techniques is known to have a significant impact on the preservation and maintenance of organic carbon (OC) levels. The primary source of soil enzymes is derived from microorganisms when compared to from plants and animals [38]. The tillage practices chosen directly and indirectly impact the biodynamics of soil. The presence of carbon in CT promotes the acceleration of soil enzyme activities, thereby contributing to the enhancement of soil biological health [39].

Moreover, conservation tillage systems foster a more significant presence of mycorrhizal fungi. The reduced disturbance and continuous presence of crop residues create favorable conditions for mycorrhizal symbiosis with plant roots. Mycorrhizal associations enhance nutrient uptake, particularly phosphorus and micronutrients, further supporting plant growth and health [40]. The utilization of computed tomography (CT) has been observed to yield positive effects and foster harmonious interactions with soil biological components. The minimal alteration of the land plays a crucial role in facilitating the establishment and development of communities, thereby fostering a harmonious equilibrium among various biological components [41, 42]. Overall, conservation tillage practices lead to a more biologically active and diverse soil ecosystem compared to conventionally plowed soils. These changes in soil biological properties contribute to improved soil health, increased nutrient availability, enhanced carbon sequestration, and, ultimately, sustainable agricultural practices.

Advertisement

10. Tillage as a tool for modification of soil ecology and modification in soil environment—a case study

The adoption of effective tillage practices is an essential requirement for the long-term maintenance of soil health and the optimization of crop production [43]. Conservation tillage (no tillage, reduced, and strip) increases soil microbial activity, moisture content of the soil, organic matter, stability of aggregates, cation exchange capacity, and crop production [44, 45]. The impact of tillage practices on soil chemical and physical properties, as well as the quality of fruits and crop yield, as documented by some studies conducted in watermelon and rice-maize cropping systems [46, 47]. By increasing plant water usage efficiency and decreasing irrigation water and labor use compared to traditional farming, conservation tillage, which makes use of permanent beds and strip tillage, has the potential to boost farmers’ net income and benefit–cost ratio. In their experiment, Kaisi et al. [48] discovered that tillage intensity greatly decreased soil macro- and microaggregate stability. Soil organic matter rose by 0.17% and soil accessible P by 3.8% in the topsoil (0–20 cm) when conservation tillage procedures were used instead of conventional tillage [49]. Maintaining crop residues on the top soil surface layer (full cover, no till; partial cover, strip tillage) can also reduce soil erosion and increase soil moisture content [50, 51]. Nevertheless, there is ongoing debate regarding the impact of different tillage practices, including conservation and conventional methods, on soil microorganisms and physical properties. The utilization of conservation tillage practices has been observed to result in an increase in the abundance of microorganisms in the soil crop system, though the amount of effectiveness is outlined by several ecological factors and field conditions [52, 53]. A 10-year study on the effects of different tillage methods on tomato yields indicated that conventional tillage (moldboard plow) resulted in 52% fewer nematodes than conservation strip tillage [54]. The fall measurements of nematode population composition in a strip tillage field revealed the following: 1900 bacterivorous, 40 fungivorous, 283 omnivorous, 37 predatory, and 1869 root-feeding (plant parasitic) worms. Moldboard plow soil had a total of 407 bacterivores, 67 omnivores, 14 predators, and 350 root-feeding nematodes, but no fungivores were found. However, the presence of nematodes does not always indicate that the soil is healthy or functioning well. For instance, in comparison to conventional tillage, strip tillage resulted in significant increases of total bacteria (49 percent), active bacteria (27 percent), active and total fungi (37 percent), and total nematodes (275 percent) [55]. In contrast to conventional tillage, strip tillage has been demonstrated in the same study to increase (9-fold) root-feeding nematodes (harmful to plant roots) and lower (possibly) soil nutrient content (P and NO3-N) [56]. Nematode feeding behavior and reproductive rate, both of which react rapidly to changes in the rhizosphere, may be a potent reason to this. Nematodes benefit more from conservation tillage because it promotes the growth of more beneficial microorganisms (bacteria and fungi) than conventional methods. Higher weed pressure management is a major drawback of conservation tillage approaches, especially no-tillage systems [57]. Soil bulk density and compaction (increased penetrometer resistance) can also increase in no-till conditions. By contrast, conventional tillage procedures improve soil structure by increasing air and water circulation, reducing compaction, and alleviating weed pressure, while also incorporating crop leftovers and nutrients [58]. Over relatively short periods of time, tillage causes substantial biophysical and biochemical changes. Direct effects on creatures include death, injury, or exposure to predators, in addition to the indirect effects of habitat destruction (Figure 1). Alterations in the tillage regime can impact the predominance of certain species, the number of populations, and the diversity of communities in the soil.

11. Future directions and research needs

One potential research gap in precision tillage is the optimization of tillage practices for sustainable agriculture. While precision tillage techniques have gained popularity due to their potential for reducing soil erosion, improving water infiltration, and increasing crop yields, there is still a need for further research to refine and optimize these practices.

Here are a few specific research areas within precision tillage/strategic tillage that could be explored:

  1. Depth control: Investigating the optimal tillage depth for different soil types, crop rotations, and field conditions could help minimize soil disturbance while still achieving desired outcomes such as weed control and residue management. Additionally, studying the effects of varying tillage depths on soil compaction and root development could provide valuable insights for precision tillage practices.

  2. Variable rate tillage: Developing algorithms and decision support tools for variable rate tillage could enhance precision in the field. This involves identifying and mapping spatial variability in soil properties, such as soil texture, organic matter content, and compaction, and using this information to prescribe varying tillage depths or intensities across the field. Evaluating the agronomic and economic impacts of variable rate tillage could help optimize its implementation.

  3. Conservation tillage and cover cropping integration: Investigating the integration of precision tillage with conservation practices like cover cropping could lead to more sustainable and environmentally friendly systems. Research could focus on determining the most effective timing and methods for terminating cover crops using precision tillage techniques, as well as assessing the impacts on soil health, nutrient cycling, and weed suppression.

  4. Soil quality and carbon sequestration: Examining the long-term effects of precision tillage on soil quality and carbon sequestration is essential for assessing its sustainability. Research could investigate the changes in soil organic matter content, microbial activity, soil structure, and nutrient availability under different precision tillage systems. Furthermore, exploring the potential of precision tillage to mitigate greenhouse gas emissions and contribute to climate change adaptation could be a valuable area of study.

  5. Economic analysis and machinery development: Assessing the economic feasibility and cost-effectiveness of precision tillage systems, including the required machinery and equipment, is crucial for adoption by farmers. Conducting economic analyses that consider the investment costs, operational expenses, and potential returns associated with precision tillage practices could provide valuable insights for farmers and policymakers. Moreover, exploring opportunities for developing and improving precision tillage machinery, such as sensors, actuators, and automation technologies, could further enhance the efficiency and effectiveness of these practices.

12. Conclusion

Throughout the centuries, tillage has been employed as a method to create a suitable seedbed for cultivating crops, as well as to manage weed growth and integrate various substances such as fertilizers, pesticides, manures, and other amendments. In the early phases, the process of converting native ecosystems through tillage played a crucial role in extracting nutrients from soil organic matter. This extraction process allowed for the utilization of naturally fertile soils to cultivate crops, thus meeting the needs of a burgeoning population with limited resources. Nevertheless, it is important to note that tillage practices have had a detrimental impact on soil organic matter and soil structure. This has resulted in an acceleration of soil erosion and the disruption of the intricate network of soil organisms [59]. In places where soil is intensively and continually farmed, the results of soil deterioration brought on by soil preparation owing to the unchecked exploitation of agricultural systems are plain to see [60].

The process of soil inversion and pulverization through repeated tillage has been found to enhance the decomposition of organic matter, thereby impacting the physical, chemical, and biological properties of the soil. These properties are considered crucial indicators of soil quality [44]. Over the course of the last three decades, there have been significant advancements in land management systems aimed at reducing the necessity for soil tillage. Methods such as no tillage are employed to maintain plant residues on the soil surface, thereby safeguarding the soil against erosion. If crop rotation is implemented in the reduced tillage system, it appears to be economically competitive with conventional tillage. Long-term benefits to local and global ecosystems are greater with the decreased tillage approach. A slower, pulsed release of nutrients for plant uptake results from the shift in decomposition rate from a microbial to a fungal route, and crop residue retention generally has a favorable effect on soil biotic complexity. When compared to regular tillage, crop residue retention reduces CO2 emissions to the environment and preserves the soil’s useful chemical and physical qualities for the long term. High crop productivity in traditional high-input agroecosystems is accomplished not through the breakdown of SOM, but rather by the use of synthetic fertilizers (mostly nitrogen, potassium, and phosphorus). Reduced retention of nitrogen and phosphorus (N and P) fertilizers and large losses of SOM in conventionally tilled systems are major problems [61].

References

  1. 1. Mrabet R. Sustainable agriculture for food and nutritional security. In: Farooq M, Gogoi N, Pisante M, editors. Sustainable Agriculture and the Environment. Cambridge, MA, USA: Academic Press; 2023. pp. 25-90
  2. 2. Wang JB, Chen ZH, Chen LJ, Zhu AN, Wu ZJ. Surface soil phosphorus and phosphatase activities affected by tillage and crop residue input amounts. Plant, Soil and Environment. 2011;57(6):251-257
  3. 3. Xu J, Han H, Ning T, Li Z, Lal R. Long-term effects of tillage and straw management on soil organic carbon, crop yield, and yield stability in a wheat-maize system. Field Crops Research. 2019;233:33-40
  4. 4. Sadiq M, Li G, Rahim N, Tahir MM. Sustainable conservation tillage technique for improving soil health by enhancing soil physicochemical quality indicators under wheat mono-cropping system conditions. Sustainability. 2021;13(15):8177
  5. 5. Raimondo M, Nazzaro C, Marotta G, Caracciolo F. Land degradation and climate change: Global impact on wheat yields. Land Degradation & Development. 2021;32(1):387-398
  6. 6. Baker JM, Ochsner TE, Venterea RT, Griffis TJ. Tillage and soil carbon sequestration—What do we really know? Agriculture, Ecosystems & Environment. 2007;118(1-4):1-5
  7. 7. Tebrugge F, During R-A. Reducing tillage intensity—A review of results from a long-term study in Germany. Soil & Tillage Research. 1999;53(1):15-28
  8. 8. Kladivko EJ. Tillage systems and soil ecology. Soil and Tillage Research. 2001;61(1-2):61-76
  9. 9. Somasundaram J, Dalal R, Lal R. Conclusions: perspectives on sustainable soil management. In: Sustainable Soil Management: Beyond Food Production. Cambridge Scholars Publishing; 2023. p. 322
  10. 10. Lamandé M, Munkholm LJ, Børresen T. Soil tillage☆, Reference Module in Earth Systems and Environmental Sciences. Elsevier; 2023
  11. 11. Hallett PD, Bengough AG. Managing the soil physical environment for plants. In: Gregory PJ, Nortcliff S, editors. Soil Conditions and Plant Growth. Chichester, UK: Wiley-Blackwell; 2013. pp. 238-268
  12. 12. Pearsons KA, Omondi EC, Zinati G, Smith A, Rui Y. A tale of two systems: Does reducing tillage affect soil health differently in long-term, side-by-side conventional and organic agricultural systems? Soil and Tillage Research. 2023;226:105562
  13. 13. Mannering JV, Fenster CR. What is conservation tillage? Journal of Soil and Water Conservation. 1983;38(3):140-143
  14. 14. Holland JM. The environmental consequences of adopting conservation tillage in Europe: Reviewing the evidence. Agriculture, Ecosystems & Environment. 2004;103(1):1-25. Available from: https://www.grainsa.co.za/conventional-vs-minimum-tillage-and-its-effect-on-soil
  15. 15. Vogeler I, Horn R, Wetzel H, Krümmelbein J. Tillage effects on soil strength and solute transport. Soil and Tillage Research. 2006;88(1-2):193-204
  16. 16. Derpsch R. The extent of conservation agriculture adoption worldwide: Implications and impact. In: Proceedings of the 3rd World Congress on Conservation Agriculture, Nairobi, Kenya, 3-7 October 2005. Harare: ACT; 2005
  17. 17. El Titi A. Implications of soil tillage for weed communities. In: El Titi A, editor. Soil Tillage in Agroecosystems. Boca Raton, FL: CRC Press; 2003. pp. 147-185
  18. 18. Blevins RL, Thomas GW, Cornelius PL. Influence of no-tillage and nitrogen fertilization on certain soil properties after 5 years of continuous corn 1. Agronomy Journal. 1977;69(3):383-386
  19. 19. Doran JW. Soil microbial and biochemical changes associated with reduced tillage. Soil Science Society of America Journal. 1980;44(4):765-771
  20. 20. Rice CW, Smith MS, Blevins RL. Soil nitrogen availability after long-term continuous no-tillage and conventional tillage corn production. Soil Science Society of America Journal. 1986;50(5):1206-1210
  21. 21. Du C, Li L, Effah Z. Effects of straw mulching and reduced tillage on crop production and environment: A review. Water. 2022;14(16):2471
  22. 22. Wardak DLR, Padia FN, de Heer MI, Sturrock CJ, Mooney SJ. Zero tillage has important consequences for soil pore architecture and hydraulic transport: A review. Geoderma. 2022;422:115927
  23. 23. Baeumer K, Bakermans WAP. Zero-tillage. Advances in Agronomy. 1974;25:77-123
  24. 24. Gupta A, Singh UB, Sahu PK, Paul S, Kumar A, Malviya D, et al. Linking soil microbial diversity to modern agriculture practices: A review. International Journal of Environmental Research and Public Health. 2022;19(5):3141
  25. 25. Anikwe MAN, Ubochi JN. Short-term changes in soil properties under tillage systems and their effect on sweet potato (Ipomea batatas L.) growth and yield in an Ultisol in South-Eastern Nigeria. Soil Research. 2007;45(5):351-358
  26. 26. Benjamin JG. Tillage effects on near-surface soil hydraulic properties. Soil and Tillage Research. 1993;26(4):277-288
  27. 27. Butorac A. Conservation tillage in eastern Europe. In: Conservation Tillage in Temperate Agroecosystems. CRC Press; 2017. pp. 357-374
  28. 28. Lal R, Reicosky DC, Hanson JD. Evolution of the plow over 10,000 years and the rationale for no-till farming. Soil and Tillage Research. 2007;93(1):1-12
  29. 29. Pagliai M, Vignozzi N, Pellegrini S. Soil structure and the effect of management practices. Soil and Tillage Research. 2004;79(2):131-143
  30. 30. McVay KA, Budde JA, Fabrizzi K, Mikha MM, Rice CW, Schlegel AJ, et al. Management effects on soil physical properties in long-term tillage studies in Kansas. Soil Science Society of America Journal. 2006;70(2):434-438
  31. 31. Fabrizzi KP, Garcıa FO, Costa JL, Picone LI. Soil water dynamics, physical properties and corn and wheat responses to minimum and no-tillage systems in the southern pampas of Argentina. Soil and Tillage Research. 2005;81(1):57-69
  32. 32. Silburn DM, Freebairn DM, Rattray DJ. Tillage and the environment in sub-tropical Australia—Tradeoffs and challenges. Soil and Tillage Research. 2007;97(2):306-317
  33. 33. Lal R. Long-term tillage and maize monoculture effects on a tropical Alfisol in western Nigeria. I. Crop yield and soil physical properties. Soil and Tillage Research. 1997;42(3):145-160
  34. 34. Rasmussen KJ. Impact of ploughless soil tillage on yield and soil quality: A scandinavian review. Soil and Tillage Research. 1999;53(1):3-14
  35. 35. Ismail I, Blevins RL, Frye WW. Long-term no-tillage effects on soil properties and continuous corn yields. Soil Science Society of America Journal. 1994;58(1):193-198
  36. 36. Dalal RC. Long term trends in total nitrogen of a vertisol subjected to zero-tillage, nitrogen application and stubble retention. Soil Research. 1992;30(2):223-231
  37. 37. Kotroczó Z, Juhos K, Biró B, Kocsis T, Pabar SA, Varga C, et al. Effect of detritus manipulation on different organic matter decompositions in temperate deciduous forest soils. Forests. 2020;11(6):675
  38. 38. Bandick AK, Dick RP. Field management effects on soil enzyme activities. Soil Biology and Biochemistry. 1999;31(11):1471-1479
  39. 39. Nugroho PA, Juhos K, Prettl N, Madarász B, Kotroczó Z. Long-term conservation tillage results in a more balanced soil microbiological activity and higher nutrient supply capacity. International Soil and Water Conservation Research. 2023;11:528-537
  40. 40. Cookson WR, Murphy DV, Roper MM. Characterizing the relationships between soil organic matter components and microbial function and composition along a tillage disturbance gradient. Soil Biology and Biochemistry. 2008;40(3):763-777
  41. 41. Engell I, Linsler D, Sandor M, Joergensen RG, Meinen C, Potthoff M. The effects of conservation tillage on chemical and microbial soil parameters at four sites across Europe. Plants. 2022;11(13):1747
  42. 42. Kurm V, Schilder MT, Haagsma WK, Bloem J, Scholten OE, Postma J. Reduced tillage increases soil biological properties but not suppressiveness against Rhizoctonia solani and Streptomyces scabies. Applied Soil Ecology. 2023;181:104646
  43. 43. Jabro JD, Stevens WB, Evans RG, Iversen WM. Tillage effects on physical properties in two soils of the Northern Great Plains. Applied Engineering in Agriculture. 2009;25:377-382
  44. 44. Cannell R, Hawes J. Trends in tillage practices in relation to sustainable crop production with special reference to temperate climates. Field Crops Research. 1994;30:245-282
  45. 45. Gozubuyuk Z, Sahin U, Ozturk I, Celik A, Adiguzel MC. Tillage effects on certain physical and hydraulic properties of a loamy soil under a crop rotation in a semi-arid region with a cool climate. Catena. 2014;118:195-205
  46. 46. Gathala MK, Timsina J, Islam MS, Rahman MM, Hossain MI, Harun-Ar-Rashid M, et al. Conservation agriculture-based tillage and crop establishment options can maintain farmers’ yields and increase profits in South Asia’s rice–maize systems: Evidence from Bangladesh. Field Crops Research. 2015;172:85-98
  47. 47. Sahu P, Singh D, Prabha R, Meena K, Abhilash P. Connecting microbial capabilities with the soil and plant health: Options for agricultural sustainability. Ecological Indicators. 2019;105:601-612
  48. 48. Al-Kaisi M, Douelle A, Kwaw-Mensah D. Soil microaggregate and macroaggregate decay over time and soil carbon change as influenced by different tillage systems. Journal of Soil and Water Conservation. 2014;69(6):574-580
  49. 49. Shao Y, Xie Y, Wang C, Yue J, Yao Y, Liu W. Effects of different soil conservation tillage approaches on soil nutrients, water use and wheat-maize yield in rainfed dry-land regions of North China. European Journal of Agronomy. 2016;81:37-45
  50. 50. Celik A, Altikat S, Way T. Strip tillage width effects on sunflower seed emergence and yield. Soil and Tillage Research. 2013;131:20-27
  51. 51. Mullins GL, Alley SE, Reeves DW. Tropical maize response to nitrogen and starter fertilizer under strip and conventional tillage systems in Southern Alabama. Soil and Tillage Research. 1998;45:1-15
  52. 52. Leskovar D, Othman Y, Dong X. Strip tillage improves soil biological activity, fruit yield and sugar content of triploid watermelon. Soil and Tillage Research. 2016;163:266-273
  53. 53. Yang S, Kim M, Seo Y, Choi K, Lee S, Kwak Y, et al. Soil microbial community analysis of between no-till and tillage in a controlled horticultural field. World Journal of Microbiology and Biotechnology. 2012;28:1797-1801
  54. 54. Overstreet L, Hoyt G, Imbriani J. Comparing nematode and earthworm communities under combinations of conventional and conservation vegetable production practices. Soil and Tillage Research. 2010;110:42-50
  55. 55. Meena VS, Verma JP, Verma SK, Sihag SK. Towards the prime response of manure to enhance nutrient use efficiency and soil sustainability a current need: A book review. Journal of Cleaner Production. 2016;112:1258-1260
  56. 56. Dotaniya M, Meena V, Basak B, Meena R. Potassium uptake by crops as well as microorganisms. In: Meena VS, Maurya BR, Verma JP, Meena RS, editors. Potassium Solubilizing Microorganisms for Sustainable Agriculture. New Delhi, India: Springer; 2016. pp. 267-280
  57. 57. Sharratt B, Zhang M, Sparrow S. Twenty years of conservation tillage research in subarctic Alaska II. Impact on soil hydraulic properties. Soil and Tillage Research. 2006;91:82-88
  58. 58. Zhang YJ, Wang S, Wang H, Ning F, Zhang Y, Dong Z, et al. The effects of rotating conservation tillage with conventional tillage on soil properties and grain yields in winter wheat-spring maize rotations. Agricultural and Forest Meteorology. 2018;263:107-117
  59. 59. Papendick RI, Parr JF. No-till farming: The way of the future for a sustainable dryland agriculture. Annals of Arid Zone. 1997;36:193-208
  60. 60. Derpsch R, Moriya K. Implications of on-tillage versus soil preparation on sustainability of agricultural production. Advances in Geoecology. 1998;31:1179-1186
  61. 61. Lal R. Soil Conservation, Reference Module in Life Sciences. Elsevier; 2017

Written By

Mahima Dixit, Debabrata Ghoshal, Sanjeev Kumar and Debashis Dutta

Submitted: 25 July 2023 Reviewed: 28 August 2023 Published: 19 June 2024