Sources Identification of Nitrogen Using Major Ions and Isotopic Tracers in Shenyang, China

Table 6

The recharge ratios of the Hun River to the groundwater.

Section	Point	Distance from Hun River (km)	G (‰)		R (‰)	P (‰)	θ (%)
I	LG18	1.02	δ^18O	−8.69	−9.14	−7.59	70.97
			δ^2H	−52.44	−66.92	−64.98	86.60
II	ZK05	0.66	δ^18O	−8.49	−9.21	−7.59	55.56
			δ^2H	−52.44	−65.7	−63.45	83.03
III	JS23-1	0.41	δ^18O	−8.80	−9.87	−8.32	30.97
			δ^2H	−54.90	−71.90	−64.90	58.82
IV	LG42-2	0.47	δ^18O	−8.88	−9.79	−8.32	38.10
			δ^2H	−54.90	−72.30	−66.00	63.79