Wavelength- and Temperature-Dependent Apparent Quantum Yields for Photochemical Production of Carbonyl Compounds in the North Pacific Ocean.

Wavelength- and Temperature-Dependent Apparent Quantum Yields for Photochemical Production of Carbonyl Compounds in the North Pacific Ocean.
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DOI:
10.1021/acs.est.7b05462
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发表时间:
2017-12
影响因子:
11.4
通讯作者:
Yuting Zhu;D. Kieber
Yuting Zhu;D. Kieber
中科院分区:
环境科学与生态学1区
文献类型:
--
作者:
Yuting Zhu;D. Kieber

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溶解有机物的光解是阳光照射下的海水中羰基化合物的主要来源,但速率和光效率受到很大的限制。测定了北太平洋海水中乙醛、乙二醛和甲基乙二醛光化学生成的波长和温度依赖的表观量子产率(AQY)。在290 ~ 380 nm波长范围内,20 °C时的波长依赖性AQY随波长的增加呈指数下降,乙醛、乙二醛和丙酮醛的AQY分别从1.29 × 10-4下降到4.12 × 10-6、2.52 × 10-5下降到6.89 × 10-7和4.37 × 10-6下降到1.25 × 10-7 mol(mol quanta)-1。AQYs在310 nm处照射6 h后下降,可能是由于光化学前体或羰基光解的耗尽。乙醛、乙二醛和甲基乙二醛在320 nm处光化学生成的平均活化能(95% CI)分别为9.31(±9.3)、26.0(±7.5)和34.7(±12.8)kJ mol-1。表层海水中光化学产生率的峰值响应为λ 325 nm,其中λ 30%来自UV-B,λ 70%来自UV-A。计算中午波长积分光产率分别为0.5-0.8,0.04-0.2,和0.03-0.06 nmol L-1 h-1的乙醛,乙二醛,和甲基乙二醛,分别在8月无云条件下。结果可用于确定这些化合物在海洋表面的区域规模的光化学生产率。
Photolysis of dissolved organic matter is the main source of carbonyl compounds in sunlit seawater, but rates and photoefficiences are poorly constrained. Wavelength- and temperature-dependent apparent quantum yields (AQYs) were determined for photochemical production of acetaldehyde, glyoxal, and methylglyoxal in North Pacific Ocean seawater. Wavelength-dependent AQYs at 20 °C decreased exponentially with increasing wavelength between 290 and 380 nm, from 1.29 × 10-4 to 4.12 × 10-6, 2.52 × 10-5 to 6.89 × 10-7, and 4.37 × 10-6 to 1.25 × 10-7 mol (mol quanta)-1 for acetaldehyde, glyoxal, and methylglyoxal, respectively. AQYs decreased after 6 h irradiation at 310 nm, possibly due to depletion of photochemical precursors or carbonyl photolysis. Average activation energies (95% CI) for photochemical production at 320 nm were 9.31 (±9.3), 26.0 (±7.5), and 34.7 (±12.8) kJ mol-1 for acetaldehyde, glyoxal, and methylglyoxal, respectively. The peak response for photochemical production rates in surface seawater was ∼325 nm, with ∼30% contribution from UV-B and ∼70% from UV-A. Computed noontime wavelength-integrated photoproduction rates were 0.5-0.8, 0.04-0.2, and 0.03-0.06 nmol L-1 h-1 for acetaldehyde, glyoxal, and methylglyoxal, respectively, under cloudless conditions in August. Results can be used to determine regional-scale photochemical production rates for these compounds in the surface ocean.