Prediction of Nano, Fine, and Medium Colloidal Phosphorus in Agricultural Soils with Machine Learning

Abstract

Soil colloids have been shown to play a critical role in soil phosphorus (P) mobility and transport. However, identifying the potential mechanisms behind colloidal P (Pcoll) release and the key influencing factors remains a blind spot. Herein, a machine learning approach (random forest (RF) coupled with partial dependence plot analyses) was applied to determine the effects of different soil physicochemical parameters on mobilizable Pcoll content in three colloidal fractions (i.e., nano- (NP): 1–20 nm, fine- (FC): 20–220 nm and medium-sized colloids (MC): 220–450 nm) based on a regional dataset of 12 farmlands in Zhejiang Province, China. RF successfully predicted mobilizable Pcoll content (R2 = 0.98). Results showed that colloidal- organic carbon (OCcoll) and minerals were the major determinants of total mobilizable Pcoll content (1–450 nm); their critical values for increasing Pcoll release were 87.0 mg L–1 for OCcoll, 11.0 mg L–1 for iron (Fecoll) or aluminium (Alcoll), 2.6 mg L–1 for calcium (Cacoll), 9.0 mg L–1 for magnesium (Mgcoll), 2.5 mg L–1 for silicon (Sicoll), and 1.4 mg L–1 for manganese (Mncoll). Among three colloidal fractions, the major factors determining Pcoll were soil Olsen-P (POlsen; 125.0 mg kg–1), Cacoll (2.5 mg L–1), and colloidal P saturation (21.0%) in NP; Mncoll (1.5 mg L–1), Mgcoll (6.8 mg L–1), and POlsen (135.0 mg kg–1) in FC; while Mncoll (1.5 mg L–1), Alcoll (2.5 mg L–1), and Fecoll (3.8 mg L–1) in MC, respectively. OCcoll had a considerable effect in the three fractions, with critical values of 80.0 mg L–1 in NP or FC, and 50.0 mg L–1 in MC. It can be concluded that the P-carrying colloidal vectors in NP are mainly OC–Ca colloids; in MC, they are mainly Fe/Al/Mn-oxyhydroxide colloids complexed with OCcoll; in FC, both phenomena likely occur.

Keywords: agricultural soils, colloidal phosphorus, soil colloids, phosphorus bioavailability, machine learning