{"title":"瓦夫洛达尔-伊尔季斯地区水体中硅、铁和氧化性的分布情况","authors":"S. Romanova, Е. Кrupa, А. Sеrikova","doi":"10.54668/2789-6323-2024-113-2-42-56","DOIUrl":null,"url":null,"abstract":"The materials of our own research on the distribution of silicon, iron and the value of permanganate oxidability in the Irtysh River basin in the summer of 2023 presented. It has been established that the content of these components and their ratios are not the same in the water of rivers and lakes. The values of permanganate oxidizability (PO) for the water of the Irtysh River in most cases did not exceed the average values for natural waters of arid zones (5…10 mgO/dm3), as well as the maximum permissible concentrations for fishery waters. The water of floodplain lakes and storage lakes is more enriched with easily oxidizing organic substances (8.62…31.51 mgO/dm3). The maximum concentrations of silicon did not always correspond to the minimum values of total mineralization. The distribution of dissolved total iron is uneven and varies between 0.072...1.740 mg/dm3, with a maximum concentration in oz. Kurkol and the Balkyldak storage lake. From the upper to the lower sections of the Ertis, there was a slight increase in the concentration of iron and silicon, as a result, of the influence of an anthropogenic factor. The assessment of the quality of the water bodies of the Pavlodar Irtysh region was carried out on the basis of a Unified water quality classification system. The relationship of the average strength between silicon, iron and the value of PO is revealed. The data on the distribution of these components can be used for a more complete assessment of the water quality of the Yertis basin.","PeriodicalId":256870,"journal":{"name":"Hydrometeorology and ecology","volume":"65 2","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-07-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"DISTRIBUTION OF THE SILICON, IRON AND OXIDIZABILITY IN THE WATER BODIES OF THE PAVLODAR ЕRTIS REGION\",\"authors\":\"S. Romanova, Е. Кrupa, А. Sеrikova\",\"doi\":\"10.54668/2789-6323-2024-113-2-42-56\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The materials of our own research on the distribution of silicon, iron and the value of permanganate oxidability in the Irtysh River basin in the summer of 2023 presented. It has been established that the content of these components and their ratios are not the same in the water of rivers and lakes. The values of permanganate oxidizability (PO) for the water of the Irtysh River in most cases did not exceed the average values for natural waters of arid zones (5…10 mgO/dm3), as well as the maximum permissible concentrations for fishery waters. The water of floodplain lakes and storage lakes is more enriched with easily oxidizing organic substances (8.62…31.51 mgO/dm3). The maximum concentrations of silicon did not always correspond to the minimum values of total mineralization. The distribution of dissolved total iron is uneven and varies between 0.072...1.740 mg/dm3, with a maximum concentration in oz. Kurkol and the Balkyldak storage lake. From the upper to the lower sections of the Ertis, there was a slight increase in the concentration of iron and silicon, as a result, of the influence of an anthropogenic factor. The assessment of the quality of the water bodies of the Pavlodar Irtysh region was carried out on the basis of a Unified water quality classification system. The relationship of the average strength between silicon, iron and the value of PO is revealed. The data on the distribution of these components can be used for a more complete assessment of the water quality of the Yertis basin.\",\"PeriodicalId\":256870,\"journal\":{\"name\":\"Hydrometeorology and ecology\",\"volume\":\"65 2\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2024-07-24\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Hydrometeorology and ecology\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.54668/2789-6323-2024-113-2-42-56\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Hydrometeorology and ecology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.54668/2789-6323-2024-113-2-42-56","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
摘要
介绍了我们自己对 2023 年夏季额尔齐斯河流域硅、铁和高锰酸盐氧化值分布情况的研究材料。研究表明,这些成分的含量及其比例在河流和湖泊中并不相同。在大多数情况下,额尔齐斯河水的高锰酸盐氧化性(PO)值不超过干旱地区天然水的平均值(5...10 毫克氧化亚氮/立方分米),也不超过渔业用水的最大允许浓度。洪泛平原湖泊和蓄水湖泊的水更富含易氧化的有机物质(8.62...31.51 毫克氧化亚氮/立方米)。硅的最大浓度并不总是与总矿化度的最小值相对应。溶解总铁的分布不均匀,介于 0.072...1.740 毫克/立方米之间,最大浓度出现在盎司、......和......。库尔科尔(Kurkol)和巴尔基尔达克(Balkyldak)蓄水湖中的浓度最高。从额尔齐斯河上游到下游,由于人为因素的影响,铁和硅的浓度略有上升。对巴甫洛达尔-额尔齐斯河地区水体质量的评估是根据统一水质分类系统进行的。研究揭示了硅、铁和 PO 值之间的平均强度关系。这些成分的分布数据可用于对叶尔季斯河流域的水质进行更全面的评估。
DISTRIBUTION OF THE SILICON, IRON AND OXIDIZABILITY IN THE WATER BODIES OF THE PAVLODAR ЕRTIS REGION
The materials of our own research on the distribution of silicon, iron and the value of permanganate oxidability in the Irtysh River basin in the summer of 2023 presented. It has been established that the content of these components and their ratios are not the same in the water of rivers and lakes. The values of permanganate oxidizability (PO) for the water of the Irtysh River in most cases did not exceed the average values for natural waters of arid zones (5…10 mgO/dm3), as well as the maximum permissible concentrations for fishery waters. The water of floodplain lakes and storage lakes is more enriched with easily oxidizing organic substances (8.62…31.51 mgO/dm3). The maximum concentrations of silicon did not always correspond to the minimum values of total mineralization. The distribution of dissolved total iron is uneven and varies between 0.072...1.740 mg/dm3, with a maximum concentration in oz. Kurkol and the Balkyldak storage lake. From the upper to the lower sections of the Ertis, there was a slight increase in the concentration of iron and silicon, as a result, of the influence of an anthropogenic factor. The assessment of the quality of the water bodies of the Pavlodar Irtysh region was carried out on the basis of a Unified water quality classification system. The relationship of the average strength between silicon, iron and the value of PO is revealed. The data on the distribution of these components can be used for a more complete assessment of the water quality of the Yertis basin.