Woo, 2016

Paper/Book

Mean Age Distribution of Inorganic Soil-nitrogen

Woo, D.K., and Kumar, P. (2016)
Water Resources Research  

Plain English Summary

The distribution of age of nitrogen in a soil column exhibits more variability than that of a nonreactive tracer.  Mean nitrogen age is lower under soybean compared to corn as it utilizes soil-nitrogen from previous years thereby reducing the mean age. Fertilizer application rapidly reduces mean-age through the soil column which subsequently increases gradually.

Abstract

Schematic representation of soil carbon and nitrogen model for the first two layers, and the last layer of the multilayer model. Boxes in the second and last layers represent the same carbon and nitrogen pools as shown in the first layer. Layers not shown follow second layer approach. This model is modified from Woo et al. [2014].

Schematic representation of soil carbon and nitrogen model for the first two layers, and the last layer of the multilayer model. Boxes in the second and last layers represent the same carbon and nitrogen pools as shown in the first layer. Layers not shown follow second layer approach. This model is modified from Woo et al. [2014].

Excess reactive nitrogen in soils of intensively managed landscapes causes adverse environmental impact, and continues to remain a global concern. Many novel strategies have been developed to provide better management practices and, yet, the problem remains unresolved. The objective of this study is to develop a model to characterize the ‘‘age’’ of inorganic soil-nitrogen (nitrate, and ammonia/ammonium). We use the general theory of age, which provides an assessment of the time elapsed since inorganic nitrogen has been introduced into the soil system. We analyze a corn-corn-soybean rotation, common in the Midwest United States, as an example application. We observe two counterintuitive results: (1) the mean nitrogen age in the topsoil layer is relatively high; and (2) mean nitrogen age is lower under soybean cultivation compared to corn although no fertilizer is applied for soybean cultivation. The first result can be explained by cation-exchange of ammonium that retards the leaching of nitrogen, resulting in an increase in the mean nitrogen age near the soil surface. The second result arises because the soybean utilizes the nitrogen fertilizer left from the previous year, thereby removing the older nitrogen and reducing mean nitrogen age. Estimating the mean nitrogen age can thus serve as an important tool to disentangle complex nitrogen dynamics by providing a nuanced characterization of the time scales of soil-nitrogen transformation and transport processes.

Citation

Woo, D.K., and Kumar, P. (2016): Mean Age Distribution of Inorganic Soil-nitrogen. Water Resources Research. DOI: 10.1002/2015WR017799

This Paper/Book acknowledges NSF CZO grant support.