Agriculture and Soil Improvement

Agriculture and Soil Improvement

Agriculture and soil improvement is the process of remediating problems such as acidity and salinity through chemical and biological methods. The main aim is to keep the soil in the 6.5-7.5 pH range for plant roots, thereby increasing yield and securing sustainable production.

What Is Soil Improvement and Why Is It Necessary?

As of 2026, soil improvement in the agricultural sector is no longer treated merely as a pH-correction or salt-removal operation; it is regarded as a strategic management process integrated with carbon sequestration, water efficiency and biodiversity goals.

In practice, liming is planned together with organic matter supplementation (green manuring, compost, farmyard manure), controlled drainage and precision agriculture data.

The sustainable agriculture approach that has come onto the agenda within the framework of the European Green Deal also positions liming as a tool that reduces nitrogen loss and greenhouse gas emissions. In Türkiye, the soil analysis and fertilization support programs run by the Ministry of Agriculture and Forestry are among the important mechanisms that carry this approach to the field level.

What Is Soil Improvement and Why Is It Necessary?

Key Problems Degrading Soil Quality in Türkiye

A significant portion of Türkiye's soils faces various types of degradation due to regional climatic differences and many years of monoculture farming.

While soils in rainy regions such as the Black Sea and Eastern Marmara are generally acidic in character, salinity, sodicity and inadequate drainage come to the fore in Central and Southeastern Anatolia.

On the coastal strips of the Aegean and the Mediterranean, salt accumulation and heavy metal risk are observed due to intensive vegetable growing and greenhouse cultivation. In fields planted with a single crop for a long time, the organic matter ratio can fall below 1%; below this threshold, the soil's buffer capacity weakens, water retention declines and the risk of wind and water erosion increases markedly.

Key Problems Degrading Soil Quality in Türkiye
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The Role of Lime-Based Solutions in Soil Improvement

On acidic soils, the most common, most economical and longest-lasting improvement method is liming; for this reason, the first intervention that comes to mind when soil improvement is mentioned is lime application.

Which type of lime is preferred depends on the soil's current pH level, its texture, the planned crop pattern and how quickly the correction needs to be completed.

Liming does not merely raise the pH; it increases the soil's buffer capacity, improves aggregation, revives microbial activity and accelerates nitrogen mineralization. The sum of these effects brings a visible improvement in fertilizer effectiveness in subsequent seasons. Hydrated lime (Ca(OH)₂), also known as slaked lime, dissolves rapidly upon contact with water and neutralizes the H⁺ ions in the soil.

The Role of Lime-Based Solutions in Soil Improvement

Technical Parameters in Liming Application

When liming is done correctly, the window of effect in the soil stays open for 3-5 years; when done incorrectly, side effects such as temporary excessive alkalinization and a decline in iron and zinc availability arise.

The main technical parameters to consider in application are: Dosage based on soil analysis: Not only pH, but also aluminum saturation, cation exchange capacity (CEC) and organic matter content must be taken into account.

While an application of 840 kg/ha may be sufficient in sandy soil, the same amount may not even provide a 1-point pH increase in clayey soil. Timing: Lime is applied 3-6 months before sowing, generally in autumn or early spring. Lime applied just before sowing can damage seed germination due to its alkaline reaction.

Technical Parameters in Liming Application

Mine Site Rehabilitation and Erosion Control

On mine sites and heavily damaged land, the soil pH is generally extremely low or unbalanced; in soils affected by acid mine drainage, the pH can drop to 2-3. On such grounds, plant establishment and ecosystem restoration are only possible with a systematic improvement program.\n\nQuicklime application rapidly raises the low pH, keeping heavy metals immobilized in the soil and unavailable for uptake by plant roots. On sloping terrain, a fine limestone aggregate layer contributes to erosion control by slowing surface runoff.\n\nIn rehabilitation projects, when liming is planned together with organic matter supplementation, green manuring and controlled drainage, soil vitality is rapidly triggered. Vişne Madencilik aggregate and lime products provide comprehensive solutions for mine site restoration.

Mine Site Rehabilitation and Erosion Control

Sustainable Soil Improvement Approach as of 2026

As of 2026, soil improvement in the agricultural sector is no longer treated merely as a pH-correction or salt-removal operation; it is regarded as a strategic management process integrated with carbon sequestration, water efficiency and biodiversity goals.

In practice, liming is planned together with organic matter supplementation (green manuring, compost, farmyard manure), controlled drainage and precision agriculture data.

The sustainable agriculture approach that has come onto the agenda within the framework of the European Green Deal also positions liming as a tool that reduces nitrogen loss and greenhouse gas emissions. In Türkiye, the soil analysis and fertilization support programs run by the Ministry of Agriculture and Forestry are among the important mechanisms that carry this approach to the field level.

Sustainable Soil Improvement Approach as of 2026

Frequently Asked Questions

Liming should generally be done in autumn or early spring, before the rains and immediately after the soil is tilled. In this way, the lime descends into the root zone with the rains and improves the soil's pH balance.
Lime should be applied to soils with a pH below 6.0, that is, soils of acidic character. Liming is essential especially in areas where acidic fertilizers such as ammonium sulfate have been used for many years.
In acidic soils, plant roots cannot take up the applied fertilizer (especially phosphorus), which becomes locked into clay minerals. When the pH is brought to the 6.5-7.5 range through liming, the uptake of nutrient elements rises to its maximum level.
Agricultural lime (CaCO₃) reacts slowly and is used in long-term improvement. Quicklime (CaO), on the other hand, gives a much faster and stronger reaction; it is preferred for soil disinfection or the urgent improvement of heavily acidic soils.
The dosage is calculated as a result of a laboratory soil analysis based on soil pH, buffer capacity, cation exchange capacity and organic matter ratio. Blind application is risky in terms of both cost and soil balance.
The ideal soil pH for lawn areas is the 6.0-7.0 range. Based on the soil analysis, 100-400 kg of hydrated lime per decare is spread and mixed to a depth of 10-15 cm. It should be done at least 2-4 weeks before sowing.
Yes. Naturally sourced limestone products (calcium carbonate and hydrated lime) are among the inputs permitted for soil improvement by organic farming certification bodies.
Yes. Applying a very high dose of lime at once raises the pH excessively and reduces the availability of micronutrient elements such as iron, zinc and manganese. For this reason, liming should never be done without analysis.
Depending on soil and climate conditions, the effect of liming lasts 3-5 years. At the end of this period, a new soil analysis is carried out to determine whether it needs to be repeated. Unnecessary consecutive applications should not be made.
Indirectly, yes. Liming strengthens soil aggregation and plant roots develop more healthily. A strong root structure and well-aggregated soil create a natural resistance to wind and water erosion.