2000
DOI: 10.2136/sssaj2000.642533x
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Inverse Estimation of Parameters in a Nitrogen Model Using Field Data

Abstract: An important step in numerical modeling is the determination of model parameters. Because of practical limitations, as well as time and financial constraints, inverse algorithms have in recent years presented an attractive alternative to direct methods of parameter estimation. In this study we linked the inverse algorithm of SUFI with the simulation program LEACHM to study N turnover of an agricultural field. Addressing the inherent modeling uncertainties, we introduce the concept of conditioned parameter dist… Show more

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Cited by 34 publications
(20 citation statements)
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“…If the NSEF value is closer to one, the efficiency of a model is higher. Sumner (2000) Air entry value (kPa) AVE -17 -0.149 Ramos and Carbonell (1991), Schmied et al (2000) Exponent for Campbell's equation BCAM 0.14 31.5 Lesikar et al (1997), Schmied et al (2000) Conductivity (mm day -1 ) K 264 13400 Ramos and Carbonell (1991), Schmied et al (2000) Dispersivity (mm) D 1 300 Ramos and Carbonell (1991) Crop data Maximum ratio of actual to potential RT 1 1.55 Acutis et al (2000), Schmied et al (2000) Relative root depth Denitrification rate (day -1 ) Kdenitr 2 9 10 -5 0.12 Johnson et al (1999), Schmied et al (2000) Residue rate (day -1 ) Kres 1.5 9 10 -3 0.01 Acutis et al (2000), Borah and Kalita (1999) Manure rate (day -1 ) Kman 8 9 10 -3 0.04 Sogbedji et al (2006), Acutis et al (2000) Humus rate (day -1 ) Khum 1.1 9 10 -5 7.5 9 10 -5 Acutis et al (2000), Schmied et al (2000) Nutr Cycl Agroecosyst (2010) Drained water at deeper soil depth is less, but the change of drainage was also smaller at deeper soil depth. Therefore they became more sensitive at deeper soil depth.…”
Section: Calibration and Validationmentioning
confidence: 99%
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“…If the NSEF value is closer to one, the efficiency of a model is higher. Sumner (2000) Air entry value (kPa) AVE -17 -0.149 Ramos and Carbonell (1991), Schmied et al (2000) Exponent for Campbell's equation BCAM 0.14 31.5 Lesikar et al (1997), Schmied et al (2000) Conductivity (mm day -1 ) K 264 13400 Ramos and Carbonell (1991), Schmied et al (2000) Dispersivity (mm) D 1 300 Ramos and Carbonell (1991) Crop data Maximum ratio of actual to potential RT 1 1.55 Acutis et al (2000), Schmied et al (2000) Relative root depth Denitrification rate (day -1 ) Kdenitr 2 9 10 -5 0.12 Johnson et al (1999), Schmied et al (2000) Residue rate (day -1 ) Kres 1.5 9 10 -3 0.01 Acutis et al (2000), Borah and Kalita (1999) Manure rate (day -1 ) Kman 8 9 10 -3 0.04 Sogbedji et al (2006), Acutis et al (2000) Humus rate (day -1 ) Khum 1.1 9 10 -5 7.5 9 10 -5 Acutis et al (2000), Schmied et al (2000) Nutr Cycl Agroecosyst (2010) Drained water at deeper soil depth is less, but the change of drainage was also smaller at deeper soil depth. Therefore they became more sensitive at deeper soil depth.…”
Section: Calibration and Validationmentioning
confidence: 99%
“…The parameters related with water movement, such as AVE and BCAM, did not exhibit any distinct trend. Schmied et al (2000) showed that six parameters related to the litter pool, its mineralization, and the denitrification rate are most sensitive for nitrate leaching using simple one-at-a time approach. Mahmood et al (2002), however, concluded that the bulk density, air entry value, BCAM, mineralization rate, base temperature, and Q10 factor are more sensitive than soil moisture content, organic carbon, and nitrification and denitrification rates.…”
Section: Calibration and Validationmentioning
confidence: 99%
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“…So-called "inverse modeling" has been widely used in uncertainty schemes over recent years (e.g. Abbaspour et al, 1999Abbaspour et al, , 2000Schmied et al, 2000;Beven and Freer, 2001;Vrugt et al, 2003, and Most of these schemes use Bayes' theorem, as this allows a "prior" distribution of uncertain input and parameter values to change in response to the amount and perceived (weighted) value of information available (Frenc and Smith, 1997;Bernado and Smith, 2001). The prior is sampled to provide a range of possible models for simulating the same problem, and uncertainties are propagated to model outputs by implementing the sample (running the models) and recording the results.…”
Section: Inverse Modelingmentioning
confidence: 99%