Shinozuka Ken'ichi, Nagafuchi Osamu, Nakazawa Koyomi, Tsunogai Urumu, Nakagawa Fumiko, Tetsuka Kenshi, Tetsuka Natsumi, Ebise Senichi
River Basin Research Center, Gifu University 1-1 Yanagido Gifu City Gifu 501-1112 Japan
Environmental Science Institute, Comprehensive Research Organizations of Fukuoka Institute of Technology Wajiro Higashi, Higashi-ku Fukuoka 811-0295 Japan.
RSC Adv. 2024 Sep 19;14(41):29860-29872. doi: 10.1039/d4ra04168b. eCollection 2024 Sep 18.
In East Asia, high levels of atmospheric nitrogen are deposited onto land. This could elevate the nitrate levels in coastal waters river runoff, even from areas where anthropogenic sources are minimal. It is important to identify NO sources in river water and the mechanisms involved in NO runoff. Yakushima Island, Japan, is a Natural World Heritage site featuring numerous watersheds with diverse topography and rivers. The area receives significant precipitation, with up to 10 000 mm in mountainous regions. Its proximity to coastal urban areas in China (∼800 km) leads to substantial atmospheric nitrogen wet and dry deposition in the island's forests. The study aimed to clarify regional water quality characteristics by conducting long-term monitoring of dissolved ion components (Na, K, Mg, Ca, F, Cl , NO , and SO ) in river waters, and to determine the effects of NO sources and watershed topography on NO behavior. Dissolved ion concentrations were obtained from a long-term monitoring (2011-2014) dataset. Cluster analysis classified runoff water from the central mountainous region into three groups: western region, other regions, and groundwater. The average NO concentration in the western region was 10.2 μmol L, which was higher than the 6.24 μmol L observed in the other regions. Stable isotope analysis in December 2018 showed that river water NO (1.39 μmol L) in the western region had a high proportion of atmospheric NO . Topographic analysis indicated that NO and atmospheric NO increased in smaller watersheds and steeper terrain. This study conclude that NO output is controlled by topography.
在东亚,大量大气氮沉降到陆地上。这可能会提高沿海水域河流径流中的硝酸盐水平,即使是在人为源极少的地区。识别河水中的氮源以及氮径流所涉及的机制很重要。日本屋久岛是一处自然世界遗产地,有众多地形多样的流域和河流。该地区降水量很大,山区可达10000毫米。它靠近中国沿海城市地区(约800公里),导致该岛森林中有大量大气氮干湿沉降。该研究旨在通过对河水中溶解离子成分(钠、钾、镁、钙、氟、氯、硝酸根和硫酸根)进行长期监测来阐明区域水质特征,并确定氮源和流域地形对氮行为的影响。溶解离子浓度取自一个长期监测(2011 - 2014年)数据集。聚类分析将中部山区的径流水分为三组:西部地区、其他地区和地下水。西部地区的平均硝酸根浓度为10.2微摩尔/升,高于其他地区观测到的6.24微摩尔/升。2018年12月的稳定同位素分析表明,西部地区河水中的硝酸根(1.39微摩尔/升)有很大比例来自大气。地形分析表明,在较小的流域和更陡峭的地形中,硝酸根和大气氮增加。本研究得出结论,硝酸根输出受地形控制。