Soil Tillage System

Last updated: June 19, 2025

Soil tillage system — a complex of scientifically substantiated tillage practices performed sequentially in crop cultivation or in the fallow field of a crop rotation to provide optimal soil conditions for plant growth and development.

Through the soil tillage system, soil regimes and phytosanitary condition are regulated, the thickness of the arable layer is increased, and the development of erosion is prevented. Tillage practices may consist of one or several technological operations; for example, chiseling allows loosening, crumbling, and partial mixing of the soil.

The soil tillage system determines the agronomic culture of the field and, as a consequence, the level of fertility and the yield of agricultural crops.

Types of Soil Tillage Systems

Depending on their purpose, soil tillage systems are divided into:

  • main;
  • pre-sowing;
  • post-sowing, for crop care.

The choice of practices constituting a specific soil tillage system is determined by landscape conditions, soil type and condition, zonal climatic characteristics, field weed infestation, preceding crops and their biological characteristics, and the fertilizer system in crop rotation. It must ensure optimal timing and high quality of work.

The following systems of mechanical tillage are used:

  • The tillage system for spring crops is determined by the preceding crop, for example, annual non-row crops of continuous sowing, row crops, sown perennial grasses, clean or coulisse fallows, tillage for intermediate crops and after their harvest.
  • The soil tillage system for winter crops includes tillage of clean, coulisse, or occupied fallows and tillage after non-fallow predecessors.
  • Tillage systems for specific crops are combined into technological complexes or soil tillage systems in crop rotation.

According to the method of main tillage for individual crops, systems are divided into:

  • moldboard;
  • non-moldboard;
  • combined;
  • minimal;
  • combination systems, including two or more tillage methods.

For example, if moldboard tillage predominates in a crop rotation and chisel tillage is also used, the system is called moldboard-chisel. If flat-cut tillage predominates in the crop rotation and alternates with moldboard tillage, it is called flat-cut-moldboard.

All tillage systems for individual crops are inextricably interrelated in crop rotation and are based on a scientifically substantiated combination of deep and shallow, moldboard and non-moldboard, and other types of tillage in each field for a specific crop. Taking into account the fertility level, field weed infestation, and other conditions, the possibility of reducing the depth and number of main tillage operations is determined; where there is a risk of erosion, soil-protective tillage is used.

Depth is a key parameter of tillage that affects the incorporation of fertilizers, seeds, and vegetative organs of weeds, as well as the quality of crumbling. Depending on depth, the following are distinguished:

  • surface — to a depth of up to 8 cm;
  • shallow — from 8 to 16 cm;
  • ordinary (medium) — from 16 to 24 cm;
  • deep — from 24 to 40 cm;
  • plantation — to a depth of more than 40 cm.

Designing a Soil Tillage System

Tillage systems for specific crops in crop rotation are interrelated because tillage for preceding crops significantly influences the features of soil preparation for subsequent crops. Therefore, all tillage systems for individual crops are combined into technological complexes or soil tillage systems in crop rotations. In crop rotation, various combinations of deep and shallow, moldboard, non-moldboard, and flat-cut tillage are used.

Scientific data on crop response to the depth of main tillage in crop rotations and the thickness of the arable layer show the need for a variable-depth tillage system, due to the alternation of plants with different thickness and depth of root system penetration, water and nutrient use, and their influence on the reproduction of fertility.

The construction of a soil tillage system in landscape agriculture is based on the following principles:

  • the principle of variable-depth tillage in crop rotation;
  • the principle of minimizing tillage;
  • the principle of soil-protective expediency and ecological adaptability of tillage practices and technologies.

On complex slopes with contour organization of the territory, tillage and sowing are carried out along the relief contours so that ridges and plant rows are located across the slope, thereby preventing water runoff and soil washout.

The construction of a soil tillage system in crop rotations must take into account preceding crops, the depth of previous tillage, and the need for deepening of the arable layer, the condition of the field surface, for example, its stoniness, soil moisture, and the number and species composition of weed vegetation.

Principle of Variable-Depth Tillage in Crop Rotation

The principle of variable-depth tillage in crop rotation substantiates the need to alternate deep, shallow, and surface tillage, taking into account the features of the agrolandscape, the biological requirements of crops, and their responsiveness to tillage depth and arable layer thickness. For example, crops with a fibrous root system predominantly located in the upper layers and insufficiently using deep soil layers respond weakly to deep tillage. Therefore, the tillage depth when these crops are placed in grain-grass, fruit-rotation, and other crop rotations, especially on fields weakly infested with perennial weeds, is up to 10–12 cm.

Crops with a taproot, deeply penetrating root system (legumes, fodder, and row crops), by contrast, respond well to deep tillage. They use the subarable layers loosened by deep tillage quite effectively. For this reason, the soil tillage system in crop rotation is built on periodic alternation of variable-depth moldboard, chisel, and other tillage operations. Variable-depth tillage allows good loosening of the “plow sole” and incorporation of seeds and vegetative organs of weed reproduction.

Principle of Minimizing Tillage

The principle of minimizing tillage is applicable primarily on well-cultivated, highly fertile soils with optimal agrophysical properties. Such soils include chernozems, chestnut, dark gray, and well-cultivated sod-podzolic soils. On such soils, the number and depth of loosening can be reduced to a minimum, and herbicides can be used to control weeds. Shallow and surface tillage are effective for winter and spring cereals, as well as intermediate crops. Zero tillage is also classified as minimal.

The main directions of tillage minimization include:

  • Reducing the number and depth of main, pre-sowing, and inter-row tillage, replacing deep tillage with surface and shallow tillage using wide-reach implements.
  • Combining several technological operations.
  • Using herbicides instead of mechanical tillage.
  • Mulching the soil with straw or green mass of green manures.
  • Sodding low-productivity soils subject to erosion risk.

Better quality of pre-sowing tillage of previously plowed soil is provided by combined units, for example, RVK-3.6, RVK-5.4, VIP-5.6, VPN-5.6, VP-8, and others. When there is no plowing, rotary tillers and rotary cultivators KFG-3.6, KA-3.6, and others are used. The use of combined machines and implements with various working parts in combination with mulching with straw and plant residues expands the possibilities of minimization, reducing the intensity coefficient to 0.46–0.56, which is especially important on erosion-hazardous lands.

Scientific data indicate the high effectiveness of minimization, which allows reducing the number of machine passes across the field, shortening work completion times, increasing labor productivity by 1.5–2 times, and reducing energy costs by 30%. Thus, reducing the depth of main tillage for winter crops from 20 to 10–12 cm reduces diesel fuel consumption by 7–10 l/ha. Minimization of tillage also has negative results: field weed infestation and plant damage by pests and diseases increase. Prolonged surface and shallow tillage lead to differentiation of fertility between the upper and lower layers, accumulation of humus and nutrients only in the upper 10-centimeter cultivated soil layer, and depletion of nitrogen and excessive compaction of the lower uncultivated layer.

Principle of Soil-Protective Expediency and Ecological Adaptability of Tillage Practices and Technologies

The principle of soil-protective expediency and ecological adaptability of tillage practices and technologies is aimed at preventing erosion processes and protecting the soil, reducing the negative impact of erosion on soil and the environment to acceptable levels. The principle is based on ecological assessment and selection of a tillage method with high erosion-control effectiveness.

In steppe agrolandscapes, the tillage system is based on non-moldboard, flat-cut, mulching tillage using loosening but non-inverting working parts such as paraplow, SibIME tines, and flat-cut implements while preserving 70–80% of stubble on the soil surface. Mulching eliminates soil overheating in summer, promotes accumulation and preservation of soil moisture, and prevents erosion.

Intensive annual soil loosening disrupts the dynamic equilibrium in the ecological system soil–plant–atmosphere. Increased aeration activates humus decomposition, destroys soil structure, and increases unproductive losses of nutrients. Thus, unproductive losses of organic carbon during crop formation amount to 40–50%. The use of non-moldboard tillage reduces this indicator to 25–30%, which positively affects the organic matter balance and increases the erosion resistance of the soil.

References

  • Bazdyrev G. I., Loshakov V. G., Puponin A. I. et al. (2000). Agriculture. Textbook for universities. Moscow: Kolos Publishing House.
  • Niklyaev V. S. (2000). Fundamentals of Agricultural Production Technology. Agriculture and Crop Production. Moscow: Bylina.
  • Evtefeev Yu. V., Kazantsev G. M. (2013). Fundamentals of Agronomy: A Textbook. Moscow: FORUM.
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