Boron contents and isotopic compositions of hog manure, selected fertilizers, and water in Minnesota
Boron contents and isotopic compositions of hog manure, selected fertilizers, and water in Minnesota
复制标题
DOI:
10.2134/jeq1997.00472425002600050004x
复制
发表时间:
1997-09
影响因子:
2.4
通讯作者:
S. Komor
中科院分区:
文献类型:
--
作者:
S. Komor
Boron-isotope (δ 11 B) values may be useful as surrogate tracers of contaminants and indicators of water mixing in agricultural settings. This paper characterizes the B contents and isotopic compositions of hog manure and selected fertilizers, and presents δ 11 B data for ground and surface water from two agricultural areas. Boron concentrations in dry hog manure averaged 61 mg/kg and in commercial fertilizers ranged from below detection limits in some brands of ammonium nitrate and urea to 382 mg/kg in magnesium sulfate. Values of δ 11 B of untreated hog manure ranged from 7.2 to 11.2‰ and of N fertilizers were -2.0 to 0.7‰. In 22 groundwater samples from a sand-plain aquifer in east-central Minnesota, B concentrations averaged 0.04 mg/L and δ 11 B values ranged from 2.3 to 41.5‰. Groundwater beneath a hog feedlot and a cultivated field where hog manure was applied had B-isotope compositions consistent with the water containing hog-manure leachate. In a 775-km 2 watershed with silty-loam soils in south-central Minnesota: 18 samples of subsurface drainage from corn (Zea mays L.) and soybean (Glycine max L. Merr.) fields had average B concentrations of 0.06 mg/L and δ 11 B values of 5.3 to 15.1‰; 27 stream samples had average B concentrations of 0.05 mg/L and δ 11 B values of 1.0 to 19.0‰; and eight groundwater samples had average B concentrations of 0.09 mg/L and δ 11 B values of -0.3 to 23.0‰. Values of δ 11 B and B concentrations, when plotted against one another, define a curved mixing trend that suggests subsurface drainage and stream water contain mixtures of B from shallow and deep groundwater.