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

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 NaHCO₃ 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.