Abstract

Soil pH effects a wide range of critical biogeochemical processes that dictate plant growth and diversity. Previous literature has established the capacity of classification and regression trees (CARTs) to predict soil pH, but limitations of CARTs in this context have not been fully explored. The current study collected soil pH, climatic, and topographic data from 100 locations across New York's Temperate Deciduous Forests (in the United States of America) to investigate the extrapolative capacity of a previously developed CART model as compared to novel CART and random forest (RF) models. Results showed that the previously developed CART underperformed in terms of predictive accuracy (RRMSE = 14.52%) when compared to a novel tree (RRMSE = 9.33%), and that a novel random forest outperformed both models (RRMSE = 8.88%), though its predictions did not differ significantly from the novel tree (p = 0.26). The most important predictors for model construction were climatic factors. These findings confirm existing reports that CART models are constrained by the spatial autocorrelation of geographic data and encourage the restricted application of relevant machine learning models to regions from which training data was collected. They also contradict previous literature implying that random forests should meaningfully boost the predictive accuracy of CARTs in the context of soil pH.

Highlights

  • Soil pH mediates provisional and regulatory service availability Soil pH, the concentration of hydrogen ions in a sample of soil, affects many critical biogeochemical processes

  • Weak significant associations were observed between soil pH and Slope (ρ = -0.31; p = 0.017) and soil pH and Terrain Ruggedness Index (TRI) (ρ = -0.33; p = 0.008)

  • We report that random forest models are not meaningfully more accurate at soil pH prediction from topographic and climatic factors than individual classification and regression trees for our study region

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Summary

Introduction

Soil pH mediates provisional and regulatory service availability Soil pH, the concentration of hydrogen ions in a sample of soil, affects many critical biogeochemical processes. These biogeochemical processes drive plant growth and diversity, which are supporting ecosystem services that sustain provisioning services (food, water, lumber, and fuel output) and regulating services (air quality, climate, erosion, and water purification) [1, 2]. Soil pH affects the metabolic quotient qCO2, which measures organic substrate uptake by soil microbes [3]. In low pH soils, higher metabolic quotients indicate increased substrate utilization by microbes (due to more costly maintenance of internal pH) and reduced carbon.

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