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Modeling Soil Test Phosphorus Changes under Fertilized and Unfertilized Managements Using Artificial Neural Networks
Author(s) -
Alvarez Roberto,
Steinbach Haydee S.
Publication year - 2017
Publication title -
agronomy journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.752
H-Index - 131
eISSN - 1435-0645
pISSN - 0002-1962
DOI - 10.2134/agronj2017.01.0014
Subject(s) - fertilizer , human fertilization , phosphorus , agronomy , soil test , environmental science , soil water , artificial neural network , mathematics , soil science , chemistry , biology , computer science , machine learning , organic chemistry
Core Ideas An artificial neural network was developed to describe soil P dynamics. The model accurately predicts soil test P increases and decreases. A meta‐model was derived to apply the build‐up and maintenance philosophy.The build‐up and maintenance criteria have been introduced for P fertilizer management in the Pampas of Argentina. However, methods for predicting soil test P changes under contrasting fertilizer rates are not available. We performed a meta‐analysis using results from 18 local field experiments performed under the most common crop rotations, in which soil test P changes with and without P fertilization and soil P balance were assessed. We assembled 329 soil test P variation data sets corresponding to a period 12 yr and 129 P balance records. The P balance was not a good predictor of annual soil test P changes ( R 2 = 0.33). In 38% of the cases, the P balance and soil test P changes showed opposite trends. Polynomial regression and artificial neural networks were tested for soil test P modeling. The neural networks performed better than the regressions ( R 2 = 0.91 vs. 0.83; P < 0.01). The network that yielded the best results used the initial soil test P level, the P fertilization rate and time as inputs. According to the model, unfertilized crops growing in soils with low initial P levels (soil test P = 10 mg kg −1 or lower) were subjected to only small decreases in soil test P levels, whereas greater decreases occurred in soils with initial high P levels. For fertilized crops, the model showed that P‐rich soils were less enriched in P than P‐poor soils. A simple meta‐model was developed for the prediction of soil test P changes under contrasting fertilizer managements.

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