Abstract

The intercropping-led diversified tillage is crucial for sustainable development in dryland agriculture. However, the plant-plant interaction transition and its effects on soil physiochemical characteristics along soil phosphorus (P) levels are not clear. To address this issue, maize-grass pea intercropping system was used to investigate the variations in plant-plant facilitation along soil P gradients (low- to high-P) and their effects on rhizosphere soil N and P availability and microbial biomass. The data showed that total net effect (NE) was always positive, indicating facilitative effects of intercropping on total community productivity. Specifically, the relative yield (RY) for both species was greater than 0.5 in the P-deficient soils, representing mutually facilitated effects. Yet, under the P-sufficient condition, maize and grass pea acted as facilitated species and facilitator respectively. Rhizosphere phosphatase activity was significantly enhanced in the P-deficient soils, accordingly fostering P mineralization for higher P availability and N utilization. The contents of microbial biomass carbon, nitrogen and phosphorus (i.e., MBC, MBN and MBP) were evidently elevated in intercropping systems than those of monoculture. Also, global meta-analysis verified above phenomenon, showing that high P addition decreased facilitation intensity with type shift, regarding plant productivity, N and P utilization and vice versa. We confirmed a relatively full picture of P-driven facilitation intensity and type shift along stress gradients by field observation and meta-analysis. The findings provided a new insight of biodiversity in soil physiochemical traits and also revealed a critical mechanism affecting resource utilization in the P-limited soils.

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