| Literature DB >> 33299027 |
Ilona Pavlovska1, Aneka Klavina2, Agris Auce2, Ivars Vanadzins2, Alise Silova2, Laura Komarovska2, Baiba Silamikele3, Linda Dobkevica4, Linda Paegle2.
Abstract
Development trends need the necessity for wider use of the local resources and available natural materials are one of the priorities around the world. Freshwater sapropel is a common material in the water basement of the lakes, but still not sufficiently explored. The main goal of the project to start detailed and systematic research on the medical properties of sapropel to be obtained in Latvia, promote its scientifically based use in balneology, develop new medical procedures and services, and promote development of new exportable products. The results include the survey, sampling depths, and processing, evaluation of external signs, physical, chemical, and biochemical parameters, and evaluation of microbiological indicators. Active components from the sapropel samples extracted using the alkaline method. Sapropel extracts were characterized by organic carbon content, humic and fulvic acid concentrations, total phenolic content, trace metal and pesticide concentrations, total antioxidant status, and microbiological flora. Summarizing the article's main findings it was concluded that Latvian freshwater sapropel can be used as raw material for obtaining sapropel extract and use it in the preparation of pharmaceuticals and promote the development of new exportable products and services.Entities:
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Year: 2020 PMID: 33299027 PMCID: PMC7725781 DOI: 10.1038/s41598-020-78498-6
Source DB: PubMed Journal: Sci Rep ISSN: 2045-2322 Impact factor: 4.379
Figure 1Sapropel extraction in Latgale District. Workers from geological research company “Geo Consultants, Ltd.” extract the samples. All pictures are the property of RSU Laboratory of Hygiene and Environmental Health, prepared in accordance with the LVS EN 1997-2 AC:2014 L (Eurocode 7—Geotechnical design—Part 2: Ground investigation and testing).
Figure 2Overview of sapropel sampling points for a specific lake. All pictures were made in cooperation with geological research company “Geo Consultants, Ltd.” and are the property of RSU Laboratory of Hygiene and Environmental Health, prepared in accordance with the LVS EN 1997–2 AC:2014 L (Eurocode 7 – Geotechnical design – Part 2: Ground investigation and testing).
Figure 3Storage of sapropel in the: (a) closed plastic containers, (b) removed from plastic containers and (c) selected samples for the extraction of active components.
Description of the lakes.
| Zeilu | Mazais Kivdalova | Ivusku | Dunakla | Audzelu | |
|---|---|---|---|---|---|
| Average depth of lake water layer (m) | 1.1 | 1.3 | 1.0 | 2.2 | 2.0 |
| Sapropel layer depth (m) | 4.0–9.5 | 1.7–11.2 | 2.2–10.4 | 0.9–9.5 | 2.65–11.4 |
| Lake surface area (h) | 44.8 | 14.7 | 1.9 | 82.7 | 64.9 |
| Lake bottom structure | Muddy | Muddy | Muddy | Muddy Gravelly | Muddy Sandy Rocky |
| Proximity of access roads (km) | 0.5 | 0.2 | 0.2 | 0.5 | 0.2 |
| Surroundings | Surrounded by reed beds, marshy forest; rural houses and service buildings; farmland; cemetery | Rural village Nuksi; rural houses with the adjacent area; field; forest | Farmland; cemetery | Close to town Ludza; one island in the lake | Populated area Vecsloboda; forest |
| Hydrological regime | Streams: 2 inflowing brooks and 6 ditches, 1 outflowing brook | Streams: 1 inflowing river and 3 ditches | Streams | Streams: 1 inflowing brook and 2 ditches, 1 outflowing river | Streams: 1 inflowing river, 1 brook and several ditches, 1 outflowing brook, |
| Sedimentological description of a section | Brownish grey to dark brown, flowing in upper layers, getting jelly-like in the lower layers, with plant residues, some H2S odour | Grey to dark brown, flowing, jelly-like with plant residues, top layers have a bit of rough sand, lower layers become denser | Predominantly yellowish-green, sometimes light brown, flowing, jelly-like, contains poorly decomposed peat admixture | Fark brown, Flowing in upper layers, getting jelly-like in deeper layers, with plant residues and well-decomposed peat impurities | Dark brown, Moderately flowing in the upper layer, the lower layer becomes extremely dense, mainly jelly-like, in deeper layers with admixture of sand and gravel |
| Additional data | Water transparency exceeding maximum depth (> 1.6 m); overgrown | Brown water lake | Overgrown | Very intense and regular water blooming; fish thirsting is observed in harsh winters; there was a Ludza bird integrated plant, later a meat processing plant nearby (water intake for economic needs (1000 m3/day) | Regular water blooming |
Lithological description of the sapropel exploration points.
Concentration of metals, humic and fulvic acids, total organic carbon and microbiology.
| Lake↓ | pH | Total concentration, mg/ml | Metal concentration, ppm | Microbiology, uncertainty ± 15,40 | ||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| TOC | HA | FA | TPC | Pb | Cd | Ni | Co | Cu | Cr | Sb | CFU/g | Isolated species | ||
| Zeilu | 7.8 | 126.4 | 160.2 | 74.3 | 77.2 | 2.60 | 0.1 | 11.8 | 5.0 | 9.9 | 20.1 | 0.3 | 2,65 × 106 | Serratia fonticola/Pseudomonas veronii/Pseudomonas chlororaphis |
| Mazais Kivdalova | 7.3 | 129.1 | 167.8 | 72.9 | 103.6 | 2.66 | 0.2 | 18.4 | 8.2 | 12.0 | 27.2 | 0.4 | 2,0 × 105 | Pseudomonas veronii |
| Ivusku | 8.0 | 106.5 | 113.1 | 76.5 | 70.3 | 3.10 | 0.2 | 3.1 | 1.7 | 3.9 | 9.1 | 0.3 | 1,1 × 105 | Paenibacillus amylolyticus/Aeromonas bestiarum |
| Dunakla | 8.0 | 104.3 | 138.4 | 44.5 | 62.4 | 5.23 | 0.2 | 15.3 | 5.7 | 9.4 | 29.4 | 0.3 | 2,3 × 107 | Aeromonas sobria/Pseudomonas marginalis,/Brevundimonas diminuta |
| Audzelu | 7.1 | 125.4 | 161.8 | 70.0 | 118.5 | 5.84 | 0.2 | 25.2 | 6.3 | 13.3 | 52.4 | 0.4 | 2,1 × 105 | Acinetobacter johnsonii |