https://www.selleckchem.com/pr....oducts/tetrathiomoly
Increases in soil C concentration (2.99 g C kg-1 year-1 ) were tightly coupled with increases in soil N concentration (0.21 g N kg-1 year-1 ) and soil CN did not vary with time since restoration. Fourier transform infrared spectroscopy results showed that the fraction of labile aliphatic C-H and carboxylate C-O (COO) compounds in the soil increased with the age of restoration and were positively correlated with soil C and N concentrations. Our results demonstrate that restoration of floodplain hydrology in montane meadows has
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