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Rainfall dissolves calcite and thenardite (Na2SO4) at the surface, infiltrates to about 1 m, and precipitates gypsum during evaporation.
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The initial source of CO2 is rainfall which subsequently dissolves carbonate ions.
The IMX-101 particles were found to dissolve slowly under simulated rainfall conditions with NQ and NTO dissolving first, leaving DNAN crystals.
A good prediction of DP was found by considering the rainfall impact on DP dissolved from apatite in surface soil.
Being located in a doline overhung by gypsum outcrops, precipitation of Ca2 + from gypsum dissolved by rainfall and biogenic CO2 is reliable.
It is well established that soluble salts can be dissolved by rainfall, and we accordingly excluded 49 leachate compositions from our analysis.
These microorganisms are released along with particles of dissolved manure during rainfall events.
The carbonates available in carbonate rocks could have been dissolved during irrigation, rainfall infiltration and groundwater movement, and added to the groundwater system with recharging water (Singh et al. 2012).
We also assessed the associations (P < 0.05) of Enterococcus geometric mean in-stream water concentrations with rainfall, solar radiation, month of year, dissolved oxygen, turbidity, and salinity concentrations in water in order to determine how other watershed variables are associated to Enterococcus geometric mean concentrations in Waipā Stream water.
We examined associations between riparian canopy cover, presence or absence of cattle, rainfall, solar radiation, month of year, dissolved oxygen, turbidity, salinity, and Enterococcus concentrations in riparian surface soils with Enterococcus geometric mean in-stream water concentrations at Waipā watershed on the north side of the Hawaiian island Kaua'i.
The tidal range, tidal condition, air temperature, 24 h antecedent rainfall, observed lines, and average concentration of dissolved total nitrogen (DTN) in the TSE for the four sampling periods (JMA 2014 2016; Osaka City 2017) are listed in Table 1.
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