{"title":"Ionic composition, source identification of rainwater, and its contribution to nutrient deposition in monsoon, over Sundarban Mangrove forest","authors":"Natasha Majumder, Monami Dutta, Abhijit Chatterjee, Sneha Bakshi, Prasun Sanyal, Madhusudan Paul, Vandana Kumari Gupta, Avanti Acharya, Sandip Kumar Mukhopadhayay","doi":"10.1007/s10874-022-09441-4","DOIUrl":null,"url":null,"abstract":"<div><p>A detailed study on potential sources, variation, and environmental effects of the rainwater ions was carried out at Lothian Island, Sundarban mangrove forest, India, during the southwest monsoon (June–September) in 2019. On an event basis, the maximum rainwater precipitation was observed 17.65 mm Day <sup>−1</sup> and a minimum of 1.02 mm Day <sup>−1</sup>. The maximum amount of total precipitation was recorded in the month of July (237 mm). The volume weighted mean (VWM) concentration shows that the total ionic composition was 93.7 μeq L<sup>−1</sup>, whereas the percentage contribution of the total ionic concentration is found to be 45.97% to anions and 54.02% to the cations. Temporal variation was observed between early (June- July) and late monsoon (August—September), which shows a high concentration of major ions in early monsoon and low concentration in late monsoon due to the washout of atmospheric particles with the frequent and increasing precipitation. The pH values of the 78% samples show neutral pH and neutralization factors (NF) followed a sequence of NF<sub>Ca</sub> ˃NF<sub>Mg</sub> ˃ NF<sub>NH4</sub> with factors of 0.77, 0.34, and 0.14 indicating Ca<sup>2+</sup> was the most potential species to balance the acidic ions (NO<sub>3</sub><sup>−</sup>, SO<sub>4</sub><sup>2−</sup>) over the study area. Source apportionment study indicates the significant influence of marine actions (long-range transport by monsoonal wind from marine origin, Sea spray, salty soil profile of mangrove) as the major source of ions over Sundarban. The rate of nutrient wet deposition in the form of rainwater was estimated and average monsoonal nitrogen flux was observed 0.87 kg ha<sup>−1</sup>where NO<sub>3</sub> contributes the most (0.60 kg ha<sup>−1</sup>). N and P deposition flux also showed a simultaneous pattern with the seasonal nutrient concentration of surrounding river water, which may be an indication of a possible contribution of atmospheric wet deposition in the spike of monsoonal nutrient concentration in river water.\n</p></div>","PeriodicalId":611,"journal":{"name":"Journal of Atmospheric Chemistry","volume":"80 2","pages":"121 - 136"},"PeriodicalIF":3.0000,"publicationDate":"2022-08-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Atmospheric Chemistry","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1007/s10874-022-09441-4","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
引用次数: 0
Abstract
A detailed study on potential sources, variation, and environmental effects of the rainwater ions was carried out at Lothian Island, Sundarban mangrove forest, India, during the southwest monsoon (June–September) in 2019. On an event basis, the maximum rainwater precipitation was observed 17.65 mm Day −1 and a minimum of 1.02 mm Day −1. The maximum amount of total precipitation was recorded in the month of July (237 mm). The volume weighted mean (VWM) concentration shows that the total ionic composition was 93.7 μeq L−1, whereas the percentage contribution of the total ionic concentration is found to be 45.97% to anions and 54.02% to the cations. Temporal variation was observed between early (June- July) and late monsoon (August—September), which shows a high concentration of major ions in early monsoon and low concentration in late monsoon due to the washout of atmospheric particles with the frequent and increasing precipitation. The pH values of the 78% samples show neutral pH and neutralization factors (NF) followed a sequence of NFCa ˃NFMg ˃ NFNH4 with factors of 0.77, 0.34, and 0.14 indicating Ca2+ was the most potential species to balance the acidic ions (NO3−, SO42−) over the study area. Source apportionment study indicates the significant influence of marine actions (long-range transport by monsoonal wind from marine origin, Sea spray, salty soil profile of mangrove) as the major source of ions over Sundarban. The rate of nutrient wet deposition in the form of rainwater was estimated and average monsoonal nitrogen flux was observed 0.87 kg ha−1where NO3 contributes the most (0.60 kg ha−1). N and P deposition flux also showed a simultaneous pattern with the seasonal nutrient concentration of surrounding river water, which may be an indication of a possible contribution of atmospheric wet deposition in the spike of monsoonal nutrient concentration in river water.
在2019年西南季风(6 - 9月)期间,对印度孙德尔本红树林洛锡安岛雨水离子的潜在来源、变化及其环境影响进行了详细研究。在事件基础上,最大雨水降水量为17.65 mm Day - 1,最小为1.02 mm Day - 1。总降水量最大的月份为7月(237 mm)。体积加权平均(VWM)浓度表明,总离子组成为93.7 μeq L−1,而总离子浓度中阴离子占45.97%,阳离子占54.02%。在季风前期(6 - 7月)和季风后期(8 - 9月),主要离子在季风前期浓度较高,在季风后期浓度较低,主要是由于降水频繁和增加导致大气颗粒物的冲刷。78%样品的pH值为中性,中和因子(NF)依次为NFCa、NFMg、NFNH4,因子分别为0.77、0.34和0.14,表明Ca2+是最可能平衡研究区域酸性离子(NO3−、SO42−)的物质。来源解析研究表明,海洋作用(海洋风的远距离输送、海雾、红树林盐渍土剖面)是孙德班地区离子的主要来源。估算了雨水形式的养分湿沉降速率,观测到平均季风氮通量为0.87 kg ha - 1,其中NO3贡献最大(0.60 kg ha - 1)。氮、磷沉降通量也与周围河流季节养分浓度呈同步变化,这可能是大气湿沉降对河流季风养分浓度峰值的可能贡献。
期刊介绍:
The Journal of Atmospheric Chemistry is devoted to the study of the chemistry of the Earth''s atmosphere, the emphasis being laid on the region below about 100 km. The strongly interdisciplinary nature of atmospheric chemistry means that it embraces a great variety of sciences, but the journal concentrates on the following topics:
Observational, interpretative and modelling studies of the composition of air and precipitation and the physiochemical processes in the Earth''s atmosphere, excluding air pollution problems of local importance only.
The role of the atmosphere in biogeochemical cycles; the chemical interaction of the oceans, land surface and biosphere with the atmosphere.
Laboratory studies of the mechanics in homogeneous and heterogeneous transformation processes in the atmosphere.
Descriptions of major advances in instrumentation developed for the measurement of atmospheric composition and chemical properties.