Modelling nitrogen leaching from overlapping urine patches

https://doi.org/10.1016/j.envsoft.2012.10.011Get rights and content

Abstract

Urine depositions have been shown to be the main source of N leaching from grazing systems and thus it is important to consider them in simulation models. The inclusion of urine patches considerably increases the complexity of the model and this can be further aggravated if the overlaps of urine patches are also considered. Overlapping urine patches are potentially important sources of N loss because the N load in these areas can be very high. In this work, we investigate a methodology to simplify the process of accounting for overlapping urine patches. We tested a two-stage approach, where, on one hand, the urine of two consecutive depositions could be aggregated and deposited at the time of the second deposition. This was called the Delayed Representation (DR) and would be useful when the delay (Td) between overlaps is short. On the other hand, if Td is sufficiently large, the depositions would become functionally independent and the urine patches could be considered separately. We called this the Independent Representation (IR). We tested this methodology by comparing simulations where the overlapping urine patches were considered explicitly and using the DR or IR in several combination of climates, soils and management options, chosen to span the likely range in New Zealand, using the Agricultural Production Systems Simulator (APSIM) model.

The results from the simulations indicated that when Td < 20 days, the DR introduced only a low, acceptable, error in simulated N leaching. When Td > 180 days, the IR was found to be acceptable in all the climates, soils and management options simulated. This left a generic window, 20 < Td < 180 days, where explicit simulations would be required. In some conditions, that window was considerably shorter. In a dry climate and shallow soil, the window was found to be 75 < Td < 180 days, while for the simulations with a wetter climate and deep soils, that window was about 70 < Td < 90 days, except for depositions in the middle of winter. These limits should apply only to long-term simulations where the user is interested in the average behaviour of the system, as considerable year-to-year variability was observed. We suggest that these windows can be used to guide the development of simulation models that include representations of urine patches under many conditions but where the soil and/or climate conditions vary markedly from those used here the analysis should be repeated.

Highlights

► Overlapping urine depositions can affect significantly the estimates of N leaching. ► APSIM simulations are used to study the effect of the interval between depositions. ► Overlaps separated by less than 20–75 days can be simulated as a single deposition. ► Overlaps separated by more than 150–180 days can be considered independent. ► These recommendations apply to soils and climates similar to those in New Zealand.

Introduction

Urine deposited by grazing ruminants is a major contributor to the high heterogeneity in soil nitrogen conditions found in pastoral systems (Haynes and Williams, 1993; Bogaert et al., 2000; McGechan and Topp, 2004; Hutchings et al., 2007). The areas affected by urine depositions receive much larger quantities of nitrogen (N) than the remaining area, typically from 500 to 1000 kg N/ha for dairy cows (Haynes and Williams, 1993). Such quantities are far in excess of the pasture's ability to take N up before leaching occurs and thus urine patches are the major sources for N loss in grazing systems (Ball and Ryden, 1984; Di and Cameron, 2002; van Groenigen et al., 2005). The N load and the timing of deposition have been shown to be important factors defining the fate of N in urine patches (Cuttle and Bourne, 1993; Shepherd et al., 2011; Snow et al., 2011).

The heterogeneity arising from the deposition of urine patches complicates the measurement of N loss from a grazed paddock (Lilburne et al., 2012). The high spatial variability makes it difficult and costly to quantify N loss from pastoral systems and means that estimates of N loss from grazed paddocks are often associated with large uncertainties. These large uncertainties are a cause for controversy when defining environmental policies and evaluating the efficacy of mitigation actions. Simulation modelling can be an effective adjunct to experimental methods for monitoring N cycling and estimating N losses. Computer models of various levels of complexity have increasingly been used to estimate N losses worldwide. Most of these models, however, do not account for field heterogeneity. This is mainly because the complexity of the modelling setup required to simulate heterogeneity presents a technical challenge in terms of computing resources (Addiscott, 1995; Hutchings et al., 2007; Wang, 2008; Romera et al., 2012). Furthermore, the importance of heterogeneity and methodologies for the use of information with uncertainty for decision making has not been well established (Beven, 2002; Lowell, 2007).

It has been shown that for estimating N leaching from systems with grazing animals it is necessary to account explicitly for the effects of urine patches (Ryden et al., 1984; Haynes and Williams, 1993; Snow et al., 2009). However, accounting for the heterogeneity created by urine depositions is not trivial. Describing such a system within models places a high demand on computing resources and has been attempted only with considerable simplifications (McGechan and Topp, 2004; Hutchings et al., 2007; Snow et al., 2009), Apart from the variability created by single urine depositions, urine overlaps can further alter the load of N deposited onto the soil and so are potentially important for defining the amount of N leached (Pleasants et al., 2007). Overlapping urine depositions on the same grazing day are likely to be minor because these overlaps typically represent a very small fraction of the grazing area (Shorten and Pleasants, 2007). However, a urine deposition affects the soil and the plants for some length of time, and leaching from a second, overlapping, urine patch deposited some weeks or months after the first deposition will be affected by the first deposition. These temporal overlaps are likely to be more significant than those occurring within the same grazing day because the probability of the overlap and therefore the area affected greatly increases. For example, Pleasants et al. (2007) using a statistical approach estimated that, at a typical 24-h grazing density of 100 cows per ha, less than 1% of the area grazed would be affected by overlapping urine patches. Considering that there would typically be about 14 grazings per year per paddock, and that in winter the animals could be mobbed with stocking densities of up to 1000 cows per ha, the proportion of a paddock that will experience delayed overlaps rises considerably. Over one year, urine depositions affect about a quarter of the area for a typical dairy farm (Pleasants et al., 2007; Moir et al., 2011) and overlaps can represent 20% of this, according to the statistical approach of Pleasants et al. (2007). Accounting for all temporal overlaps would result in a rapid increase in modelling complexity and thus simplifications are needed. While these issues are of most interest for intensively grazed systems where the animals graze the pastures year round, the principles are applicable to grazing situations in general.

The purpose of this study was to investigate options for simplifying the representation of overlapping urine patches in the simulation modelling of grazed systems. While the work here is presented in the context of New Zealand soils and climates, the concepts are generally applicable to any grazed system. We used outputs from the simulation model Agricultural Production Systems Simulator (APSIM) to identify the nature of the interactions between successive urine depositions and how this interaction is affected by the interval between depositions. We hypothesise that when the delay (Td) between overlaps is short, the first deposition can be delayed and aggregated with the second deposition without significant error; we call this the Delayed Representation (DR). At higher values of Td, urine patches become functionally independent because the N from the first urine patch is depleted before the second is deposited and in this case, the urine patches can be considered separately with an Independent Representation (IR). We test these simplifications by comparing simulations employing DR and IR against simulations where the overlapping urine patches are considered explicitly (Explicit Representation, ER) in the same simulation. We analyse whether it is possible to define general rules for simplifying the description of urine patch overlaps using DR and IR.

Section snippets

The APSIM model

The APSIM modelling framework (Keating et al., 2003; Holzworth et al., 2010), version 7.3, was used to simulate N leaching from urine depositions in a pastoral system. The primary modules that are relevant for this work are described briefly below. SWIM (Verburg et al., 1996) models soil water dynamics using the Richards' and convection–dispersion equations with a Freundlich isotherm to simulate solute adsorption onto the soil particles. Soil N (Probert et al., 1998) calculates the C and N,

Impact of urine depositions on pasture and soil

Urine depositions affect both pasture and soil conditions, with the effects depending on many factors including the time of deposition. Fig. 2 shows the effect of single depositions in March (late summer/early autumn), June (mid-winter), September (spring) and December (summer) 1990 for the irrigated Lismore soil in the Lincoln environment with high fertiliser input. There was no increase in pasture growth following the March deposition, compared to the simulations that had not yet received a

Conclusions

Previous experimental (e.g. Ball and Ryden, 1984) and modelling work (e.g. Snow et al., 2009) has shown that the effect of urine patches is important to leaching from grazed systems. However, the inclusion of explicit urine patches in simulation models considerably increases the complexity of the model. This complexity is further aggravated if the overlaps of urine patches must also be considered. Here, we tested a two-stage methodology to simplify the account of two overlapping urine patches.

Acknowledgements

This work was supported by the Ministry for Science and Innovation through the programme “Dairy Systems for Environmental Protection”. The authors wish to thank the anonymous reviewers for their constructive comments that improved the manuscript.

References (56)

  • P.R. Ball et al.

    Nitrogen relationships in intensively managed temperate grasslands

    Plant Soil

    (1984)
  • K. Beven

    Towards a coherent philosophy for modelling the environment

    Proc. R. Soc. Lond. A – Math.

    (2002)
  • N. Bogaert et al.

    Within-field variability of mineral nitrogen in grassland

    Biol. Fert. Soils

    (2000)
  • R. Cichota et al.

    A functional evaluation of virtual climate station rainfall data

    N. Z. J. Agric. Res.

    (2008)
  • R. Cichota et al.

    Describing the Fate of High Dose Nitrogen in Pastoral Soils – Modelling N Leaching Under High N Loads (Urine Patches)

    (2010)
  • R. Cichota et al.

    Modelling the effect of a nitrification inhibitor on N leaching from grazed pastures

    Proc. N. Z. Grass. Assoc.

    (2010)
  • M.E. Close et al.

    Field study of pesticide leaching in an allophanic soil in New Zealand. 2: Comparison of simulations from four leaching models

    Aust. J. Soil Res.

    (2003)
  • B.R. Cullen et al.

    Simulating pasture growth rates in Australian and New Zealand grazing systems

    Aust. J. Agric. Res.

    (2008)
  • S.P. Cuttle et al.

    Uptake and leaching of nitrogen from artificial urine applied to grassland on different dates during a growing season

    Plant Soil

    (1993)
  • Dennis, S.J., 2009. Nitrate Leaching and Nitrous Oxide Emission from Grazed Grassland: Upscaling from lysimeters to...
  • H.J. Di et al.

    Nitrate leaching and pasture production from different nitrogen sources on a shallow stoney soil under flood-irrigated dairy pasture

    Aust. J. Soil Res.

    (2002)
  • H.J. Di et al.

    Nitrate leaching losses and pasture yields as affected by different rates of animal urine nitrogen returns and application of a nitrification inhibitor – a lysimeter study

    Nutr. Cycl. Agroecosyst.

    (2007)
  • A.E. Hewitt

    New Zealand Soil Classification

    (1998)
  • C.J. Hoogendoorn et al.

    Nitrogen concentration in the urine of cattle, sheep and deer grazing a common ryegrass/cocksfoot/white clover pasture

    N. Z. J. Agric. Res.

    (2010)
  • S.F. Ledgard

    Nitrogen cycling in low input legume-based agriculture, with emphasis on legume/grass pastures

    Plant Soil

    (2001)
  • F.Y. Li et al.

    Modelling seasonal and geographical pattern of pasture production in New Zealand

    N. Z. J. Agric. Res.

    (2011)
  • L. Lilburne et al.

    Computer-based evaluation of methods to sample nitrate leached from grazed pasture

    Soil Use Manag.

    (2012)
  • K.E. Lowell

    At what level will decision-makers be able to use uncertainty information?

  • Cited by (33)

    • Application of grazing land models in ecosystem management: Current status and next frontiers

      2019, Advances in Agronomy
      Citation Excerpt :

      Extensive studies have evaluated N leaching from urine patches, including overlapping patches and uncertainty in soil properties (Cichota et al., 2013; Vogeler et al., 2017b). For example, Cichota et al. (2013), using the APSIM model, studied N leaching from grazing systems in New Zealand and found that when urine was deposited on the same location twice within 20 days, N in the two urine events should be accumulated and treated as a single urine patch. However, when the delay between the two urine events was > 180 days, independent patch simulation is sufficient for N leaching.

    View all citing articles on Scopus
    View full text