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<title>Soil Science</title>
<link>http://hdl.handle.net/10386/2797</link>
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<pubDate>Sun, 12 Apr 2026 13:34:17 GMT</pubDate>
<dc:date>2026-04-12T13:34:17Z</dc:date>
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<title>Evolving role of synthetic cytokinin 6-benzyl adenine for drought stress tolerance in soybean (Glycine max L. Merr.)</title>
<link>http://hdl.handle.net/10386/4710</link>
<description>Evolving role of synthetic cytokinin 6-benzyl adenine for drought stress tolerance in soybean (Glycine max L. Merr.)
Mangena, Phetole
The enhanced growth and productivity of soybeans during the past decades&#13;
were possible due to the application of agrichemicals such as bio-fertilizers,&#13;
chemical fertilizers, and the use of high yielding, as well as disease resistant&#13;
transgenic and non-transgenic varieties. Agrichemicals applied as seed&#13;
primers, plant protectants, and growth regulators, however, had a diminutive&#13;
significance on growth and productivity improvements across the globe.&#13;
The utilization of plant growth regulators (PGRs) for vegetative growth,&#13;
reproduction and yield quality improvements remains unexplored, particularly,&#13;
the use of cytokinins such as 6-benzyl adenine (6-BAP) to improve soybean&#13;
response to abiotic stresses. Therefore, an understanding of the role of 6-BAP&#13;
in the mediation of an array of adaptive responses that provide plants with&#13;
the ability to withstand abiotic stresses must be thoroughly investigated. Such&#13;
mitigative effects will play a critical role in encouraging exogenous application&#13;
of plant hormones like 6-BAP as a mechanism for overcoming drought stress&#13;
related effects in soybean. This paper discusses the evolving role of synthetic&#13;
cytokinin 6-bezyl adenine in horticulture, especially the implications of its&#13;
exogenous applications in soybean to confer tolerance to drought stress.
Journal article published in Journal of Frontiers in Sustainable Food Systems DOI 10.3389/fsufs.2022.992581
</description>
<pubDate>Sat, 01 Jan 2022 00:00:00 GMT</pubDate>
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<dc:date>2022-01-01T00:00:00Z</dc:date>
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<title>Infiltration-excess runoff properties of dryland floodplain soil types under simulated rainfall condition</title>
<link>http://hdl.handle.net/10386/2813</link>
<description>Infiltration-excess runoff properties of dryland floodplain soil types under simulated rainfall condition
Dlamini, P.; Mavimbela, S. S. W.; Van Rensburg, L.
The study estimated infiltration-excess runoff properties of three floodplain soil-types under aquifer water management at Anglo American Kolomela Iron Ore mine in Postmasburg, Northern Cape Province of South Africa. Rainstorm regimes of amounts 60 (high), 30 (medium), and 15 (low) mm with respective intensities of 1.61, 0.52, and 0.27mm min 1 were simulated on 1 m2 plot with 1% slope. Infiltration-excess runoff properties were affected by a rainstorm, but not soil-type. When combined with rainstorm, soil-type affected accumulative run-off rates. High rainstorm had different (p 0.05) accumulative runoff rates (0.1–0.61mm min 1) and increased with clay content. Different response times of 4, 10, and 17min for respective high, medium, and low rainstorms were quickest on higher clay plus silt content and bulk-density under high and lower rainstorms, respectively. Lower rainstorms had similar effects on accumulative runoff rates (0.01–0.05mm min 1), total runoff yield (0.59–18mm), and runoff coefficients (4.29–18%). Under the high rainstorm, total runoff yields (11.4–25.8mm) and runoff coefficients (19–42.9%) were different and increased with clay plus fine-silt content. Although simulated rainstorms had constant intensities, results showed high rainstorms to be of primal influence on infiltrationexcess runoff. Clay plus silt content and bulk-density influenced infiltration-runoff properties for respective high and lower rainstorms. Apart from rainstorm characteristics, surface clay plus silt content and bulk-density are important for harnessing surface runoff in floodplains for aquifer recharge.
Article published in the Arid Land Research and Management , DOI: 10.1080/15324982.2018.1531441
</description>
<pubDate>Mon, 01 Jan 2018 00:00:00 GMT</pubDate>
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<dc:date>2018-01-01T00:00:00Z</dc:date>
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