Changes in soil phosphorus fractions following sole cropped and intercropped maize and faba bean grown on calcareous soil

• Published in: Plant and soil Vol. 448; no. 1-2; pp. 587 - 601
• Main Authors: Liao, Dan, Zhang, Chaochun, Li, Haigang, Lambers, Hans, Zhang, Fusuo
• Format: Journal Article
• Language: English
• Published: Cham Springer International Publishing 01.03.2020; Springer; Springer Nature B.V
• Subjects: Agricultural practices; Analysis; Beans; Biomedical and Life Sciences; Broad beans; Calcareous soils; Coexistence; Corn; Cropping systems; Crops; Depletion; Ecology; Fractionation; Intercropping; Legumes; Life Sciences; Mimosaceae; Phosphorus; Phosphorus content; Plant Physiology; Plant Sciences; Regular Article; Sodium bicarbonate; Sodium hydroxide; Soil analysis; Soil dynamics; Soil investigations; Soil Science & Conservation; Soils; Sole cropping; Maize; Faba bean; Hedley fractionation; Soil phosphorus fractions; Intercropping
• ISSN: 0032-079X; 1573-5036
• DOI: 10.1007/s11104-020-04460-0

Aims This study aimed to investigate the effects of coexistence with faba bean, a phosphorus (P)-efficient crop, on soil-accumulated P use by a maize/faba bean intercropping system on dynamic changes in soil P pool. Methods Maize and faba bean were grown in P-accumulated soil as either sole cropping or intercropping. After one year (Stage I) or four years (Stage II) of no P application, soil samples were collected respectively and analyzed for soil P pools using sequential fractionation. Aboveground biomass and P content were annually measured from 2013 to 2016 to assess the annual P balance. Results The intercropped maize/faba bean system showed a P-uptake advantage, with a Land Equivalent Ratio (LER) ranging from 1.2 to 1.5. The average shoot P content over the four years in intercropped maize and faba bean was significantly greater than that of the corresponding sole crops by 29% and 30%, respectively. Over the three-year P depletion period, the three cropping systems primarily depleted the 1 M HCl-P i fraction, followed by sole maize, which depleted the NaOH-P i and concentrated HCl-P o fractions. Sole faba bean depleted the alkali-soluble P o fraction (extracted by NaHCO 3 and NaOH), and the intercropped maize/faba bean system depleted the conc. HCl-P o fraction, which was similar to the effect of sole maize. Conclusions Both sole crops and intercrops mainly depleted 1 M HCl-P i , but differed in P o depletion. Sole maize and maize/faba bean intercropping depleted the sparingly labile P o fraction, while sole faba bean depleted the labile and moderately labile P o fractions.