Journal of Environmental Quality ( IF 2.4 ) Pub Date : 2020-04-14 , DOI: 10.1002/jeq2.20068 Jennifer A. Cooper , George W. Loomis , David V. Kalen , Jose A. Amador
J.A. Cooper, G.W. Loomis, D.V. Kalen, & J.A. Amador. (2015). J. Environ. Qual . 44:953–962. https://doi.org/10.2134/jeq2014.06.0277
We discovered an error in our article, involving the use of an incorrect value for the ideal gas law constant, R , of 1.08205, instead of the correct value 0.08205. We also discovered an incorrect conversion from moles of N2O to moles of N, 1 mole N/mole of N2O was used instead of the correct value of 2 moles of N/mole of N2O). The incorrect value of R and mole conversion were used in N2O gas flux calculations. This affects a number of values presented in the article, noted below, although the changes do not have a material effect on interpretation of the results or the implications of the study.
Error on p. 956 :
In Equation 1, the correct value for R is 0.08205, not 1.08205.
Error on p. 959 :
Old incorrect text: The flux of N2O was significantly higher from SND (63 μg N m−2 h−1) and GEO (55 μg N m−2 h−1) than from P&S (3 μg N m−2 h−1).
Corrected text (changes in bold): The flux of N2O was significantly higher from SND (1653 μg N m−2 h−1) and GEO (1453 μg N m−2 h−1) than from P&S (86 μg N m−2 h−1).
Error on pp. 959–960 :
Old incorrect text: We calculated a mass balance for N entering and exiting the drainfields to help quantify loss pathways (Fig. 4). In P&S, outputs (514 g N m−2 yr−1) of N accounted for 87.6% of inputs (588 g N m−2 yr−1) to the drainfield, with 12.4% (74 g N m−2 yr−1) unaccounted for. Loss of N occurred mainly as dissolved N species, comprised of NO3 (83%), organic N (16%) and NH4 (1%). Nitrous oxide in gas and dissolved phases accounted for 0.04% of N outputs, suggesting N2O production was not a major loss pathway in P&S.
Nitrogen was better accounted for in SND and GEO, with outputs (2194 and 2170 g N m−2 yr−1) accounting for 95.1 and 94.1% of inputs (2306 g N m−2 yr−1), respectively. Loss of N occurred mainly as dissolved N species, comprised of NO3 (84–85%), organic N (14–15%) and NH4 (<1%). Nitrous oxide in the gas and dissolved phase accounted for 0.08% of N loss in SND and GEO, indicating this was not an important pathway for net N loss in either drainfield type.
Corrected text (changes in bold): We calculated a mass balance for N entering and exiting the drainfields to help quantify loss pathways (Fig. 4). In P&S, outputs (515 g N m−2 yr−1) of N accounted for 87.6% of inputs (588 g N m−2 yr−1) to the drainfield, with 12.4% (73 g N m−2 yr−1) unaccounted for. Loss of N occurred mainly as dissolved N species, comprised of NO3 (83%), organic N (16%) and NH4 (1%). Nitrous oxide in gas and dissolved phases accounted for 0.2% of N outputs, suggesting N2O production was not a major loss pathway in P&S.
Nitrogen was better accounted for in SND and GEO, with outputs (2208 and 2182 g N m−2 yr−1) accounting for 95.8 and 94.6 % of inputs (2306 g N m−2 yr−1), respectively. Loss of N occurred mainly as dissolved N species, comprised of NO3 (84–85%), organic N (14–15%) and NH4 (<1%). Nitrous oxide in the gas and dissolved phase accounted for 0.6–0.7% of N loss in SND and GEO, indicating this was not an important pathway for net N loss in either drainfield type.
中文翻译:
勘误到:评估常规和高级基于土壤的现场废水处理系统的水质功能
JA Cooper,GW Loomis,DV Kalen和JA Amador。(2015)。J.环境。资格赛。44:953–962。https://doi.org/10.2134/jeq2014.06.0277
我们在文章中发现了一个错误,涉及使用理想气体定律常数R的不正确值1.08205,而不是正确值0.08205。我们还发现从N 2 O摩尔到N摩尔的不正确转化,使用1摩尔N /摩尔N 2 O代替了正确的2摩尔N /摩尔N 2 O值。在N 2 O气体通量计算中使用了不正确的R和摩尔转化率值。尽管这些更改对结果的解释或研究的含义没有实质性的影响,但这影响了本文中提出的许多价值,如下所述。
p错误。956:
在公式1中,R的正确值为0.08205,而不是1.08205。
p错误。959:
旧的错误文本: SND(63μgN m -2 h -1)和GEO(55μgN m -2 h -1)的N 2 O通量明显高于P&S(3μgN m -2 h)-1)。
纠正的文本(以粗体显示): N中的磁通2 O的从SND显著更高(1653 微克n×m个-2 ħ -1)和GEO(1453 微克n×m个-2 ħ -1)比从P&S(86 微克Ñ m -2 h -1)。
pp。959–960出现错误:
旧的不正确的文字:我们计算了N进入和离开排水区的质量平衡,以帮助量化损失途径(图4)。在P&S中,N的输出量(514 g N m -2 yr -1)占流失场的输入量(588 g N m -2 yr -1)的87.6%,占12.4%(74 g N m -2 yr -1)- 1)无法解释。N的流失主要是溶解的N物种,包括NO 3(83%),有机N(16%)和NH 4(1%)。气相和溶解相中的一氧化二氮占氮产量的0.04%,表明N 2 O的产生不是P&S的主要损失途径。
氮在SND和GEO中的占比更好,产出(2194 g N m -2 yr -1和2194 g N m -2 yr -1)分别占输入的95.1%和94.1%(2306 g N m -2 yr -1)。N的损失主要是溶解的N物种,包括NO 3(84-85%),有机N(14-15%)和NH 4(<1%)。气相和溶解相中的一氧化二氮占SND和GEO中N损失的0.08%,表明这不是两种流失类型中N净损失的重要途径。
更正的文本(粗体更改):我们计算了N流入和流出排水区的质量平衡,以帮助量化损失途径(图4)。在P&S中, N的输出量(515 g N m -2 yr -1)占流失场的输入量(588 g N m -2 yr -1)的87.6%,占12.4%(73 g N m -2 yr -1)- 1)无法解释。N的流失主要是溶解的N物种,包括NO 3(83%),有机N(16%)和NH 4(1%)。气相和溶解相中的一氧化二氮占氮产量的0.2%,表明N 2产氧量不是P&S中的主要损失途径。
氮在SND和GEO中的占比更好,产出(2208和2182 g N m -2 yr -1)分别占输入(2306 g N m -2 yr -1)的95.8和94.6%。N的损失主要是溶解的N物种,包括NO 3(84-85%),有机N(14-15%)和NH 4(<1%)。气相和溶解相中的一氧化二氮占SND和GEO中N损失的0.6-0.7%,表明这不是两种流失类型中N净损失的重要途径。