Effect of long-term irrigation patterns on phosphorus forms and distribution in the brown soil zone

Liu, Chang; Dang, Xiuli; Mayes, Melanie A.; Chen, Leilei; Zhang, Yulong; Das, Anup

doi:10.1371/journal.pone.0188361

Title: Effect of long-term irrigation patterns on phosphorus forms and distribution in the brown soil zone

Journal Article · Mon Nov 20 00:00:00 EST 2017 · PLoS ONE

DOI:https://doi.org/10.1371/journal.pone.0188361· OSTI ID:1462832

Liu, Chang ^[1]; Dang, Xiuli ^[1];

^[1]; Chen, Leilei ^[2]; Zhang, Yulong ^[1]; Das, Anup ^[3]

Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States)
Chifeng Environmental Monitoring Central Station, Inner Mongolia (China)
ICAR Research Complex for NEH Region (India)

Continuous application of P fertilizers under different irrigation patterns can change soil phosphorus (P) chemical behavior and increase soil P levels that are of environmental concern. To assess the effect of long-term different irrigation patterns on soil P fractions and availability, this study examined sequential changes in soil organic P and inorganic P from furrow irrigation (FI), surface drip irrigation (SUR), and subsurface drip irrigation (SDI) in the brown soil zone (0–60 cm) during 1998 to 2011. Analyses of soil P behavior showed that the levels of total P are frequently high on top soil layers. The total P (TP) contents of the entire soil profiles under three irrigation treatments were 830.2–3180.1 mg/kg. The contents of available P (AP) were 72.6–319.3 mg P/kg soil through soil profiles. The greatest TP and AP contents were obtained within the upper soil layers in FI. Results of Hedley’s P fractionation indicate that HCl-P is a dominant form and the proportion to TP ranges from 29% to 43% in all three methods. The contents of various fractions of P were positively correlated with the levels of total carbon (TC), total inorganic carbon (TIC), and calcium (Ca), whereas the P fractions had negative correlation with pH in all soil samples. Regression models proved that NaHCO₃-P_o was an important factor in determining the amount of AP in FI. H₂O-P_o, NaHCO₃-P_o, and NaOH-P_i were related to available P values in SUR. NaHCO₃-P_o and NaOH-P_o played important roles in SDI. The tomato yield under SUR was higher than SDI and FI. The difference of P availability was also controlled by the physicochemical soil properties under different irrigation schedule. Here, SUR was a reasonable irrigation pattern to improve the utilization efficiency of water and fertilizer.

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Research Organization:: Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)

Sponsoring Organization:: USDOE

Grant/Contract Number:: AC05-00OR22725

OSTI ID:: 1462832

Journal Information:: PLoS ONE, Vol. 12, Issue 11; ISSN 1932-6203

Publisher:: Public Library of ScienceCopyright Statement

Country of Publication:: United States

Language:: English

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Cited by: 13 works

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