We can think of soil as a very complex solution of chemicals. There are inorganic and organic elements present in varying quantities, depending on how local climate and geology have affected soil development over time. No two soils are therefore exactly alike: all are products of their environments. Adding to the complexity is that most inorganic elements, such as micronutrients plants need, occur in different oxidation states within soils. That is micronutrients in the soil may be more likely to possess a certain electron configuration, which affects their bonding with other compounds. For plants, micronutrients are only usable in certain oxidation states because of bonding properties present from specific electron configurations. Thus we use the broad term micronutrient deficiency to describe a plant that is negatively affected by the lack of a certain micronutrient in the soil, or the inability of the plant to obtain the element from the soil.
Nutrient availability chart. https://www.pioneer.com |
Luckily plants can modify surrounding soil pH from the roots to make certain micronutrients such as iron more available. We can see this below using a chemical to stain for reduced iron that is available to plants. The Rhododendron seedling roots on top slightly lowered the media pH, while the one on the bottom lowered media pH more drastically. Note the greater saturation of the purple color on the top indicating a greater amount of reduced iron in the media. Photo credit: Elsa Eshenaur.
Hopefully this puts the mechanisms of the project in perspective. It is our goal to see how different soils have driven root adaptation to enhance iron acquisition in our research species. All in an attempt to illuminate and improve the reactions that occur beneath our feet.