2016
DOI: 10.2136/vzj2016.07.0061
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Estimating Nitrate Leaching to Groundwater from Orchards: Comparing Crop Nitrogen Excess, Deep Vadose Zone Data‐Driven Estimates, and HYDRUS Modeling

Abstract: Large spatial and temporal variability in water flow and N transport dynamics poses significant challenges to accurately estimating N losses form orchards. A 2-yr study was conducted to explore nitrate (NO 3 − ) leaching below the root zone of an almond [Prunus dulcis (Mill.) D. A. Webb] orchard. Temporal changes in water content, pore water NO 3 − concentrations and soil water potential were monitored within and below the root zone to a soil depth of 3 m at eight sites, which represented spatial variations in… Show more

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Cited by 66 publications
(44 citation statements)
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“…A recent study by Baram et al. [27] estimated leaching loss of 80-240 kg N/ha y from an almond (Prunus dulcis) orchard irrigated with micro-sprinklers, and most of the loss occurred early in the growing season (February-May), when urea-ammonium nitrate fertilizer was commonly applied to wet soil. Thus, high-frequency DI and fertigation could potentially reduce fertilizer losses and protect groundwater quality [17,28].…”
Section: Introductionmentioning
confidence: 99%
“…A recent study by Baram et al. [27] estimated leaching loss of 80-240 kg N/ha y from an almond (Prunus dulcis) orchard irrigated with micro-sprinklers, and most of the loss occurred early in the growing season (February-May), when urea-ammonium nitrate fertilizer was commonly applied to wet soil. Thus, high-frequency DI and fertigation could potentially reduce fertilizer losses and protect groundwater quality [17,28].…”
Section: Introductionmentioning
confidence: 99%
“…Numerous studies of N budget analysis in agricultural fields [25][26][27][28][29][30] concluded that the nitrate leaching could be substantial and depends mainly on the rate of applied fertilizer, source of N, soil types, and the amount of rainfall water.Nitrogen is present in the soil in nine different forms, including intermediaries of subsequent transformations, corresponding to different oxidative states [31,32]. HYDRUS software (developed by [33]) is widely used as a finite element model for simulating the movement of water, N transport, and the transformation process in variably saturated soil [34][35][36][37]. The governing convection-dispersion solute transport equations are written in a relatively general form by including provisions for non-linear, non-equilibrium reactions between the solid and liquid phases and linear equilibrium reactions between the liquid and gaseous phases [36].…”
mentioning
confidence: 99%
“…Similar K s values measured on bedrock samples were reported by Katsura, Kosugi, Yamamoto, and Mizuyama (). Although the low permeability layer was thin and its water storage had little effect on the overall soil storage, its hydraulic conductivity defined the leaching potential of the entire soil profile (Baram et al, ). The calibrated K s of the purple soil was smaller than those reported by others (Long, Liu, & Liu, ) for both cultivated and uncultivated purple sloping soils.…”
Section: Discussionmentioning
confidence: 99%