Dec 11, 2024
Soil Health – Bray’s Nutrient Mobility Concept and Immobile Plant Nutrients
Nutrient Mobility Concept
In a recent article published in this newsletter on 27 November 2024, Volume 15, No. 24, I presented an article addressing soil health and the Bray Nutrient Mobility Concept in relation to mobile nutrients (Silvertooth, 2024). In this article, the concept of nutrient behavior in soil-plant systems focuses on the immobile plant nutrients.
Plant nutrient management is strongly dependent on nutrient mobility in the soil. Nutrient mobility in the soil is different among the essential plant nutrients and nutrient management in the field needs to take this into account.
In 1954, Dr. Roger H. Bray at the University of Illinois proposed a nutrient mobility concept that has proven to be very important in the management of nutrients for optimum efficiency (agronomically, economically, and environmentally). Bray essentially simplified all soil nutrient chemistry to the fact that some plant nutrients are mobile in the soil and some are not. (Bray, 1954; Raun, 2017; Warren et al., 2017, Havlin et al. 2014; Troeh and Thompson, 2005).
Mobile Nutrients and the Root System Sorption Zone
Mobile plant nutrients in the soil move with the soil water. Thus, plants can extract mobile nutrients from a large volume of soil beyond the direct root system. Accordingly, plants take up mobile nutrients from a “root system sorption zone” (Figure 1). This gives plants the capacity to utilize most of the mobile nutrients in the root system sorption zone as those nutrients will move to the plant roots with the soil water as it is taken up by the plant (Silvertooth, 2024).
We consider the mobile plant nutrients to be nitrogen (N), sulfur (S), boron (B), and chlorine (Cl). These mobile plant nutrients are taken up by the plant in the following forms: nitrate-nitrogen (NO3--N), sulfate-sulfur (SO42- - S), boric acid (H3BO3) and borate ions (BO33- - B), and chlorine is taken up as the chloride ion (Cl-).
Figure 1. The root system sorption zone and an illustration of the large volume of soil
from which plants extract mobile nutrients.
In a crop field where many plants are growing together, there are commonly root system sorption zones commonly overlap. Therefore, the root system sorption zones for adjoining plants are competing for water and mobile nutrients, (Figure 2). This is one of the main reasons that appropriate plant populations are important for optimum yield.
Figure 2. Competition among plants brought about by increasing yield goal.
Immobile Nutrients
Plant nutrients that are immobile in the soil include phosphorus(P), potassium (K), calcium (Ca), magnesium (Mg), iron (Fe), zinc (Zn), manganese (Mn), copper (Cu), and molybdenum (Mo). Immobile nutrients do not move as freely in the soil solution as the mobile nutrients do. These nutrients interact more directly with soil colloids and root surfaces.
Immobile nutrients are absorbed by the plant from the soil and soil solution that is directly next to the root surface. Plant roots must grow through the soil volume to come into direct contact with the immobile nutrients.
Thus, only a small volume of soil and soil solution that immediately adjacent to the root surface will be involved in providing immobile nutrients to the plant. Figure 3 describes this soil volume and plant root interface as the root surface sorption zone.
Figure 3. The root surface sorption zone and an illustration of the small volume of soil
from which plants extract immobile nutrients.
In the case of immobile nutrients, the entire soil volume is not as important as the soil colloid surfaces and soil solution next to the root surface. The concentration of immobile nutrients on the soil colloids immediately next to the root surface is a critical of the root system sorption zone.
Since only a thin layer of soil surrounding and in direct contact with the plant roots are involved in supplying immobile nutrients to the plant, there is little or no competition among plants for immobile nutrients. Competition among plants only occurs at points where roots from adjacent plants come in direct contact with one another (Figure 4).
Figure 4. Limited competition among plants for immobile nutrients.
Due to this manner of immobile nutrient behavior and interaction with plant roots, the supply or concentration of immobile nutrients such as phosphorus (P) or potassium (K), is not dependent on a yield goal. In the case of immobile nutrients, the overall soil concentration of the immobile nutrients is most important, and these nutrients are not moving readily with soil water. If the immobile nutrient supply in the soil is adequate for optimum yield of a crop, the healthy plant root system can explore new soil volume and extract the nutrient sufficiently, such as phosphorus (P) or potassium (K).
The nutrient mobility concept and these basic illustrations can help us understand the basis for some common observations and resultant crop management practices. Fertilizers with immobile plant nutrients are more effective when they are incorporated into soil and particularly in soil zones where there is a high probability of plant roots encountering the immobile nutrients.
Banded applications of immobile nutrients are generally more effective than the same rates broadcast and incorporated into the soil. In contrast, mobile nutrients like nitrogen (N) can be broadcast and moved into the root system sorption zone by water.
Soil tests for immobile nutrients do not normally change much from year to year and this is true irrespective of the crop yields from the previous season or fertilizer rate. This is because most of soil volume was not in direct contact with the plant roots. Soil concentrations of immobile nutrients do not usually change rapidly but they can be slowly mined out of the soil by a series of crops without proper fertilization.
Continued or over-applications of immobile nutrient fertilizers, such as phosphorus (P), will cause a buildup of that nutrient in the soil. This is because only a small fraction (commonly 15-20% for most crops) of the nutrient or fertilizer comes into direct contact with the plant roots. The remaining amount of fertilizer interacts with the soil.
Appropriate soil tests that are properly correlated and calibrated with crop-specific response categories are important in evaluating immobile plant nutrient status. Immobile nutrient levels in the soil are commonly expressed in terms of percent sufficiency to produce a specific crop based on appropriate soil test results.
Our goal in plant nutrition management is to achieve the highest levels of efficiency (agronomically, economically, and environmentally) in the field as possible
References:
Bray, R.H.1954. A Nutrient Mobility Concept of soil-plant relationships. Soil Sci. 78(1), p. 9-22.
Havlin, J.L., Beaton, J.D., Tisdale, S.L. and Nelson, W.L. 2014. Soil Fertility and Fertilizers; An Introduction to Nutrient Management. 6th Edition, Prentice Hall, Upper Saddle River, NJ.
Silvertooth, J.C. 2024. Soil Health - Bray’s Nutrient Mobility Concept and Mobile Plant Nutrients University of Arizona Vegetable IPM Newsletter, Volume 15, No. 24,
Raun, W.R. 2017. In: Warren et al. 2017. Oklahoma Soil Fertility Handbook, Id:E-1039
Troeh, F.R. and Thompson, L.M. (2005) Soils and Soil Fertility. Sixth Edition, Blackwell, Ames, Iowa, 489.
Warren, J., H. Zhang, B. Arnall, J. Bushong, B. Raun, C. Penn, and J. Abit. 2017. Oklahoma Soil Fertility Handbook. Id: E-1039
Weil, R.R. and Brady, N.C. (2017) The Nature and Properties of Soils. 15th Edition, Pearson, New York.