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The Student's t-test did not detect differences in SOC concentration between the two soil types.
Analysis of variance indicated significant differences in soil organic carbon (P < 0.05) and soil moisture (P < 0.01) contents between the two soil geomorphological units, and field tests showed differences in soil texture and structure.
The bacterial community richness and diversity indices were calculated (Table 4); no significant differences observed between the two soil samples.
The separation of species associated with sandstone vs. alluvial soils corresponds with a large difference in P availability between the two soil types but total soil N likewise is lower on the sandstone soils [32].
Only O. lacteum differed significantly between the two soil types (40.6 ± 5.9 vs. 78.8 ± 5.0, P = 0.02).
However, we cannot exclude that the lack of effect of soil type is due to differences other than the availability of iron between the two soil types.
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Rill erosion differed between the two soils.
After oxalate or H2O2 treatment, the difference in crack patterns between the two soils became smaller.
However, there was no significant difference in bacterial diversity and richness between the two soils at day 200, indicating that long-term straw amendment probably lessens the difference in bacterial community structure between the two soils.
A comparative study on rill erosion between the two soils is important to increase research knowledge and exchange application experiences.
In the presence of stubble with identical moisture level, we observed higher bacterial diversity and richness in long-term organic manure-fertilized soil compared with the unfertilized soil at days 20 and 80, which we attributed to the different quality and quantity of organic matter between the two soils.
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