ArticleFrontiers in plant science2021
Soybean Root Growth in Response to Chemical, Physical, and Biological Soil Variations.
Article in Frontiers in plant science, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 5 papers.
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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
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Who cites it
5 citing papers in PubMed.
- Controlled-release potassium sulfate combined with the deep banding method on soybean productivity and soil microbial characteristics.Frontiers in plant science · 2026Article
- Short-Term Effects ofMicroorganisms · 2024Article
- Article
- Effects of Different Land Use Patterns on Soil Water in Loess Hilly and Gully Regions of China.Plants (Basel, Switzerland) · 2022Article
- Physiology and metabonomics reveal differences in drought resistance among soybean varieties.Botanical studies · 2022Article
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Authors and funding
7 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
Environmental conditions affect crop yield, and water deficit has been highlighted by the negative impact on soybean grain production. Radicial growth in greater volume and depth can be an alternative to minimize losses caused by a lack of water. Therefore, knowledge of how soybean roots behave before the chemical, physical, and biological attributes of the soil can help establish managements that benefit in-depth root growth. The objective was to evaluate the growth of soybean roots in response to chemical, physical, and biological variations in the soil, in different soil locations and depths. Six experiments were conducted in different locations. Soil samples were collected every 5 cm of soil up to 60 cm of soil depth for chemical, physical, and biological analysis. The roots were collected every 5 cm deep up to 45 cm deep from the ground. The six sites presented unsatisfactory values of pH and organic matter, and presented phosphorus, potassium, and calcium at high concentrations in the first centimeters of soil depth. The total porosity of the soil was above 0.50 m
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