Abstract

Knowledge of how many sampling points are needed to estimate the mean content of soil nutrients in agricultural fields, given a precision requirement on the estimated mean, is limited. This paper describes a versatile geostatistical simulation approach for predicting the variance of the mean nitrate-N (NO3-N) content within an agricultural field estimated by random sampling. In fall of 2016 sixteen agricultural fields were sampled on a square grid to model the spatial variation of NO3-N. On twelve out of sixteen fields NO3-N showed a lognormal distribution rather than a normal distribution. Variograms for (log-transformed) NO3-N are estimated using a Bayesian approach, resulting in 100 vectors with possible variogram parameters per field, obtained by MCMC sampling from the posterior distribution. Each of these variograms is used to simulate 100 maps of NO3-N, resulting in 100 × 100 maps of NO3-N per field. Each map is used to compute the variance of the estimated mean with stratified simple random sampling of 5,10,…,50 points, with one point per compact geographical stratum. For each sample size (number of sampling points) the mean, median and P90 of the uncertainty distribution are computed. Based on the medians, the sample size required for a maximum expanded measurement uncertainty of 50% varies from <5 to >50. This large variation in required sample size shows the large variation among the sixteen fields in variance of NO3-N within a field.

Highlights

  • In a world where the demand for agricultural produce is predicted to increase with 50% by 2050 (United Nations, 2017), the need for sub­ stantial improvements in both crop production and sustainable use of agricultural resources is of utmost importance

  • This paper describes a versatile geo­ statistical simulation approach for predicting the variance of the mean nitrate-N (NO3-N) content within an agricultural field estimated by random sampling

  • To get an idea of the extent of the variability of NO3-N within a field, the variability was calculated as the coefficient of variation (CV) of all measurements made on a field

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Summary

Introduction

In a world where the demand for agricultural produce is predicted to increase with 50% by 2050 (United Nations, 2017), the need for sub­ stantial improvements in both crop production and sustainable use of agricultural resources is of utmost importance. Within any programme to develop site specific management in order to increase crop yield, basic knowledge of the fertility status on the field scale plays an important role. Despite numerous studies that show the importance of sampling procedures inspired by the specific characteristics of the measurands, improved procedures tend to be neglected in favour of long-time practice or easeof-use. This results in sub optimal laboratory samples and subsequent analytical results (Starr et al, 1992; Clay et al, 1997; Hennart et al, 2004). NO3-N leaches into ground- and surface water causing eutrophication and poses a direct health risk in those areas where the population is dependent on natural water for use as drinking water, e.g. overly use of NO3-N fertilisers has been proposed

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