TY - JOUR

T1 - Using isotope fractionation of nitrate-nitrogen and nitrate-oxygen for evaluation of microbial denitrification in a sandy aquifer

AU - Böttcher, J.

AU - Strebel, O.

AU - Voerkelius, Susanne

AU - Schmidt, H. L.

N1 - Funding Information: We thank the Deutsche Forschungsgemeinschaft for providing financial support to this study.

PY - 1990/5

Y1 - 1990/5

N2 - The nitrate input into the groundwater from forest and agricultural land in the 'Fuhrberger Feld' catchment area is virtually completely degraded by microbial denitrification in the aquifer. Five multilevel groundwater sampling wells show characteristic depth functions of nitrate, proving the denitrification process. A series of 10 samples of 'arable land groundwater' was taken from different depths at these multilevel wells and isotope ratios of 15N 14N and 18O 16O in the nitrate were measured. The sampling was based on the two-dimensional vertical-plane groundwater flownet and on the knowledge of the landuse upgradient of the multilevel wells. High nitrate concentrations are associated with low δ15N and low δ18O values, and vice versa. The δ15N δ18O ratio indicates a linear increase with a slope of 1:2.1. The microbial dentrification accords with a Rayleigh process with calculated enrichment factors of ε = -15.9‰ for 15N and ε = -8.0 ‰ for 18O. Three samples taken from groundwater recharged under coniferous forest show deviating characteristics: low nitrate concentrations with low δ15N values (1-4‰) but very high δ18O values (40-50‰). Using the previously quantified enrichment factors for 15N and 18O, an attempt was made to ascertain the significance of denitrification in specific depth sections at two other multilevel wells (7 samples). In two cases quantitative assessments on the degree of nitrate concentration decrease owing to denitrification were possible. However, in other cases the specific nitrate isotope fractionation was masked by the variability of nitrate concentration and of nitrate isotope ratios in the corresponding groundwater recharge preventing definite interpretations.

AB - The nitrate input into the groundwater from forest and agricultural land in the 'Fuhrberger Feld' catchment area is virtually completely degraded by microbial denitrification in the aquifer. Five multilevel groundwater sampling wells show characteristic depth functions of nitrate, proving the denitrification process. A series of 10 samples of 'arable land groundwater' was taken from different depths at these multilevel wells and isotope ratios of 15N 14N and 18O 16O in the nitrate were measured. The sampling was based on the two-dimensional vertical-plane groundwater flownet and on the knowledge of the landuse upgradient of the multilevel wells. High nitrate concentrations are associated with low δ15N and low δ18O values, and vice versa. The δ15N δ18O ratio indicates a linear increase with a slope of 1:2.1. The microbial dentrification accords with a Rayleigh process with calculated enrichment factors of ε = -15.9‰ for 15N and ε = -8.0 ‰ for 18O. Three samples taken from groundwater recharged under coniferous forest show deviating characteristics: low nitrate concentrations with low δ15N values (1-4‰) but very high δ18O values (40-50‰). Using the previously quantified enrichment factors for 15N and 18O, an attempt was made to ascertain the significance of denitrification in specific depth sections at two other multilevel wells (7 samples). In two cases quantitative assessments on the degree of nitrate concentration decrease owing to denitrification were possible. However, in other cases the specific nitrate isotope fractionation was masked by the variability of nitrate concentration and of nitrate isotope ratios in the corresponding groundwater recharge preventing definite interpretations.

UR - http://www.scopus.com/inward/record.url?scp=0025573493&partnerID=8YFLogxK

U2 - 10.1016/0022-1694(90)90068-9

DO - 10.1016/0022-1694(90)90068-9

M3 - Article

AN - SCOPUS:0025573493

VL - 114

SP - 413

EP - 424

JO - Journal of hydrology

JF - Journal of hydrology

SN - 0022-1694

IS - 3-4

ER -