Abstract

Tillage is a critical soil management option that affect many soil physical, chemical and biological properties, which in turn may alter the soil environment and consequently impact on root growth and distribution, and crop yield. This study was carried out to evaluate the long-term effects of different soil tillage systems on some soil physical properties under both irrigated and rainfed wheat productions for nine consecutive wheat seasons (2011-12 and 2019-20) at Koont research farm, PMAS-Arid Agriculture University, Rawalpindi. Four soil tillage systems were performed i.e. conventional tillage system (S1), reduced tillage system-1 (S2), reduced tillage system-2 (S3) and no tillage system (S4). The results showed that soil moisture content measured at both soil depths (0-15 and 15-30 cm) was the maximum in direct sowing (S4) and lowest in conventional soil tillage system (S1). Bulk density and porosity were changes with tillage depth. Among studied tillage systems, bulk density and penetration resistance values were the maximum and porosity was lowest in direct wheat sowing system. Soil particle size distribution was affected by operations and agricultural machinery used in soil tillage systems. The aggregate size smaller than 1 mm showed higher fragmentation (42.25%) in S3. This study showed that soil physical properties were influenced by tillage systems in wheat production under irrigation and rainfed environment. Although the climate of the study area is semi-arid and direct sowing system provide maximum moisture but reduced tillage method can be used for better soil physical properties and highest crop yield.

Highlights

  • Tillage is one of fundamental agro-technical operations in an agricultural process applied to regulate and maintain the physical, chemical and biological balances of soil properties

  • The effect of different tillage – sowing methods on soil physical properties were examined and variance analysis values are given in Table 1 and average comparison values are given in Figure 2–3–4 and 5

  • Direct sowing (S4) system showed maximum soil moisture content measured at both soil depths (0-15 and 15-30 cm) while, lowest in conventional soil tillage system (S1)

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Summary

Introduction

Tillage is one of fundamental agro-technical operations in an agricultural process applied to regulate and maintain the physical, chemical and biological balances of soil properties. The aim of tillage in crop production is to produce favorable physical conditions for seed germination and plant growth (Jabro et al, 2011). An intensive soil tillage can lead to degradation of soil structure, due to the gradual loss of stable aggregates, leading to soil erosion and compaction, which will result in low moisture availability for plants (Castellini and Ventrella, 2012). This may affect plant nutrient availability, growth and root proliferation. Bulk density, in a loamy soil in a semiarid region with a cool

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