Header image

No-Tillage in a Maize-Based Cropping System Leads to Soil Compaction in the Topsoil Layer of a Sandy Textured Soil in a Semi-Arid Region

Tracks
Wednesday, July 23, 2025
4:38 PM - 4:50 PM

Overview

Seome Michael Swafo | University of Limpopo


Speaker

Agenda Item Image
Mr Seome Michael Swafo
Student
University of Limpopo

No-Tillage in a Maize-Based Cropping System Leads to Soil Compaction in the Topsoil Layer of a Sandy Textured Soil in a Semi-Arid Region

Abstract

In recent times, there has been a growing recognition of the field-based problems associated with sandy soils in agroecosystems. Amongst these, is soil compaction which causes soil degradation and adversely affects crop growth. However, we know relatively little about how conservation agricultural (CA) practices influence the compactibility of sandy soils in maize-based cropping systems. Our study was formulated to assess the presence and degree of soil compaction on a sandy textured topsoil under CA practices in a semi-arid region of South Africa. Treatments were laid out in a randomised complete block design with tillage as the main factor and cropping systems as the subplot factor. Tillage systems were conventional tillage (CT) and no tillage (NT) and cropping systems included (i) maize-maize-maize (MMM), (ii) wheat-fallow-maize (WFM), (iii) soybean-cover crop-soybean (SCCS) and (iv) maize-maize-cover crop (MMCC) rotation. From the treatment combinations, we determined soil physical properties; bulk density (BD), packing density (PD), total porosity (TP), relative gas diffusion coefficient (RGDC), void ratio (VR) and soil compactness degree (SCD). In comparison to CT, we found that NT significantly increased BD, PD and SCD by 3% to 918%, suggesting that minimal soil disturbance under NT results in the consolidation and densification of the sandy textured soil (90% sand content). Such alterations of the physical quality of the soil led to the reduction in TP (6%), RGDC (14%), and VR (10%) under NT relative to CT plots. This deterioration of the physical quality of the soil could negatively influence soil water retention and aeration, subsequently altering root growth, decreasing uptake of nutrients and water from the soil, especially under semi-arid regions.

Biography

Seome Michael Swafo is a PhD Candidate in Soil Science at the University of Limpopo, South Africa, where he also earned his BSc and MSc in Agriculture (Soil Science). His research focuses on sustainable land management and soil degradation in rural agricultural systems. He has published in peer-reviewed journals, serves as a reviewer for international publications, and is actively involved in professional bodies including the Soil Science Society of South Africa, the Canadian Society of Soil Science, and the International Union of Soil Science. He also contributes to teaching Soil Physics, Mineralogy, and Chemistry at both undergraduate and postgraduate levels. Mr. Swafo is the Founder, President, and Principal Soil Scientist of the Emmarentia Agriculture Institute NPC, where he leads platforms such as the Emmarentia Agricultural Science Society and the Emmarentia Journal Exchange. He also heads ModMar Soil Systems, a consultancy focused on practical, field-based solutions to soil fertility, land degradation, and sustainable agriculture. Originally from Badimong village in Limpopo Province, he is deeply committed to advancing soil science that responds to the needs of African farming communities, with an emphasis on improving land productivity and long-term agricultural sustainability.
loading