Key Laboratory of Marine Environmental Science and Ecology, Ocean University of China, Ministry of Education of China, Qingdao 266100, China.
Key Laboratory of Marine Environmental Science and Ecology, Ocean University of China, Ministry of Education of China, Qingdao 266100, China; Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China.
Sci Total Environ. 2023 Jun 1;875:162655. doi: 10.1016/j.scitotenv.2023.162655. Epub 2023 Mar 8.
Accurate assessments of soluble phosphorus (P) in aerosol particles are essential to understand the atmospheric nutrients supply to the marine ecosystem. We quantified total P (TP) and dissolved P (DP) in the aerosol particles collected in the sea areas near China in a cruise mission from May 1 to June 11, 2016. The overall concentrations of TP and DP were 3.5-99.9 ng m and 2.5-27.0 ng m, respectively. When the air originating from the desert areas, TP and DP were 28.7-99.9 ng m and 10.8-27.0 ng m, respectively, and P solubility was 24.1-54.6 %. When the air influenced mainly by anthropogenic emissions from eastern China, TP and DP were 11.7-12.3 ng m and 5.7-6.3 ng m, respectively, and P solubility was 46.0-53.7 %. More than half of the TP and more than 70 % of the DP were from pyrogenic particles, with a considerable DP converted via aerosol acidification after the particles met humid marine air. On average, aerosol acidification promoted the fractional solubility of dissolved inorganic P (DIP) to TP from 22 % to 43 %. When the air originating from the marine areas, TP and DP were 3.5-22.0 ng m and 2.5-8.4 ng m, respectively, and P solubility was 34.6-93.6 %. About one-third of the DP was from biological emissions in organic forms (DOP), leading to higher solubility than in the particles from continental sources. These results reveal the dominance of inorganic P in TP and DP from the desert and anthropogenic mineral dust and the significant contribution of organic P from marine sources. The results also indicate the necessity to treat aerosol P carefully according to different sources of the aerosol particles and atmospheric processes the particles experience in assessing aerosol P input to seawater.
准确评估气溶胶颗粒中的可溶解磷 (P) 对于了解大气向海洋生态系统供应营养物质至关重要。我们在 2016 年 5 月 1 日至 6 月 11 日的一次巡航任务中,定量分析了在中国海域采集的气溶胶颗粒中的总磷 (TP) 和溶解磷 (DP)。TP 和 DP 的总浓度分别为 3.5-99.9ng/m 和 2.5-27.0ng/m。当空气源自沙漠地区时,TP 和 DP 的浓度分别为 28.7-99.9ng/m 和 10.8-27.0ng/m,P 的可溶性为 24.1-54.6%。当空气主要受到来自中国东部的人为排放物影响时,TP 和 DP 的浓度分别为 11.7-12.3ng/m 和 5.7-6.3ng/m,P 的可溶性为 46.0-53.7%。超过一半的 TP 和超过 70%的 DP 来自于热成因颗粒,在这些颗粒遇到潮湿的海洋空气后,相当一部分 DP 通过气溶胶酸化转化而来。平均而言,气溶胶酸化将溶解无机磷 (DIP) 在 TP 中的分数溶解度从 22%提高到 43%。当空气源自海洋地区时,TP 和 DP 的浓度分别为 3.5-22.0ng/m 和 2.5-8.4ng/m,P 的可溶性为 34.6-93.6%。大约三分之一的 DP 来自海洋源生物排放的有机形式 (DOP),其可溶性高于来自大陆源的颗粒。这些结果表明,无机 P 在来自沙漠和人为矿物尘埃的 TP 和 DP 中占主导地位,而海洋源有机 P 的贡献显著。这些结果还表明,在评估气溶胶 P 对海水的输入时,需要根据气溶胶颗粒的不同来源和颗粒经历的大气过程,仔细对待气溶胶 P。