scholarly journals Ecological and geological soil assessment of the Loshamye Lake catchment area (national park “Smolensk Lakeland”)

2020 ◽  
Vol 579 ◽  
pp. 012015
Author(s):  
I I Podlipskiy ◽  
P S Zelenkovskiy ◽  
S V Dubrova ◽  
V R Hohryakov
Keyword(s):  
Catchment Area ◽  
National Park ◽  
Soil Assessment ◽  
Lake Catchment

Long-term changes in water quality and ecological status of lakes in the Wielkopolska National Park and its buffer zone with special reference to effectiveness of the lakes’ protection

2016 ◽  
Vol 45 (4) ◽  
Author(s):  
Agnieszka E. Ławniczak
Keyword(s):  
Water Quality ◽  
Catchment Area ◽  
National Park ◽  
Ecological Status ◽  
Buffer Zone ◽  
Field Studies ◽  
Long Term Changes ◽  
Protection Strategies

AbstractThis paper evaluates water quality and ecological status of lakes located in the Wielkopolska National Park and its buffer zone. Changes in water quality were analyzed from 1974 to 2012 in order to assess the effectiveness of the protection strategies implemented on the studied lakes since 1957, i.e. the date when the park was established. The ecological status of the lakes was assessed with the use of macrophytes as well as hydromorphological and physicochemical analyses performed in 2012. Changes in water quality of the studied lakes within the last 40 years were analyzed based on available published and unpublished data, as well as field studies. All water bodies are characterized by advanced eutrophication. However, evaluation of the ecological status showed good status of the charophyte-dominated lakes, i.e. Lake Wielkowiejskie and Lake Budzyńskie. Lack of significant differences in physicochemical water qualities between the park and its buffer zone indicated that measures implemented to protect the water, particularly in the park, are ineffective. This study shows that more radical conservation measures are necessary to protect and improve the water quality, not only in WPN and its buffer zone but also in the whole catchment area.

scholarly journals Investigation of the effect of anthropogenic land use on the Pănăzii Lake (Romania) catchment area using Cs-137 and Pb-210 radionuclides

PLoS ONE ◽  
2021 ◽  
Vol 16 (6) ◽  
pp. e0251603
Author(s):  
Robert-Csaba Begy ◽  
Codrin F. Savin ◽  
Szabolcs Kelemen ◽  
Daniel Veres ◽  
Octavian-Liviu Muntean ◽  
...  
Keyword(s):  
Land Use ◽  
Soil Erosion ◽  
Sedimentation Rate ◽  
Catchment Area ◽  
Gamma Spectroscopy ◽  
Soil Parameters ◽  
Erosion Rates ◽  
Soil Erosion Rate ◽  
Soil Erosion Rates ◽  
Lake Catchment

The problem of soil degradation has accentuated over recent decades. Aspects related to soil erosion and its relation to changes in land use as well as anthropogenic influence constitute a topic of great interest. The current study is focused on a soil erosion assessment in relation to land use activities in the Pănăzii Lake catchment area. Fallout radionuclides were used to provide information on soil erosion as well as redistribution rates and patterns. Variations in the sedimentation rate of the lake were also investigated as these reflect periods in which massive erosion events occurred in the lake catchment area. The novelty of this study is the construction of a timescale with regard to the soil erosion events to better understand the relationship between soil erosion and land use activities. In this study, 10 soil profiles and one sediment core from the lake were taken. Soil parameters were determined for each sample. The activities of 210Pb, 137Cs and 226Ra were measured by gamma spectroscopy. For low 210Pb activities, measurements via 210Po using an alpha spectrometer were performed. Soil erosion rates were determined by the 137Cs method and the sedimentation rate calculated by the Constant Rate of Supply (CRS) model. A soil erosion rate of 13.5 t·ha-1·yr-1 was obtained. Three distinct periods could be observed in the evolution of the sedimentation rate. For the first period, between 1880 and 1958, the average deposition rate was 9.2 tons/year, followed by a high deposition period (1960–1991) of 29.6 tons/year and a third period, consisting of the last 30 years, during which the sedimentation rate was 15.7 tons/year. These sedimentation rates fluctuated depending on the main land use activity, which can also be seen in the soil erosion rates that had almost doubled by the time agricultural activities were performed in the area.

scholarly journals Soils and sediments of Prošće Lake catchment as a possible terrigenous input in the lakes system

2020 ◽  
Vol 49 (1) ◽  
Author(s):  
Anita Ptiček Siročić ◽  
Stanislav Kurajica ◽  
Dragana Dogančić ◽  
Nikolina Fišter
Keyword(s):  
National Park ◽  
Natural Phenomenon ◽  
Northwestern Part ◽  
Valuable Insight ◽  
Absorption Bands ◽  
Recharge Area ◽  
Soils And Sediments ◽  
Lake Catchment ◽  
Dominant Phase ◽  
Plitvice Lakes

The Plitvice Lakes National Park is in the northwestern part of the Dinaric Karst in central Croatia. An important role of the soil in the karst is to purify the waters before they reach the phreatic zone. The soil is also a zone of accumulation, transformation, retardation and dilution of a potential pollutant. Knowing soil mineralogical composition is an important factor in understanding fate and transport of contaminants throughout lakes system. Samples of soil, peat and stream sediment were collected in the Prošće lake catchment and partly in the assumed zone of influence, X-ray diffraction (XRD) and Fourier Transform Infrared spectroscopy (FTIR) analysis of samples was performed to determine dominant mineral species in samples. XRD analysis showed predominance of lowquartz, which was found in all samples, most often as dominant phase. Dolomite was found in half of the samples, almost always as a significant phase while calcite was dominant phase in one of the samples. In most of the samples, members of the feldspars and chlorites groups, as well as muscovite, were present as minor phases. The absorption bands in the range of 2800-3000 cm-1 due to the organic matter are visible in spectra of all samples. These minerals can enter lakes system by surface waters, primarily streams and overland flow during snow thawing and rain, and also in cases of shore erosion. Terrigenic input in lakes is small but cannot be neglected due to the longlasting preservation efforts of the Prošće Lake recharge area, and the Plitvice Lakes National Park in general, terrigenous intake still does not pose a threat to water quality and tufa production. Considering the analyzed samples and characteristics of detected soil constituents, soils and sediments in the Prošće Lake catchment have the ability to retain and purify water on its way to the lakes. On the other hand, in case of the possible contamination in the recharge area of the lakes system, the pollutants can enter the system adsorbed on the soil particles. Learning more about the soils surrounding lakes gives valuable insight into their possible influence on lakes water chemistry and adds one piece of the puzzle into understanding this kind of a natural phenomenon.

Living with Fire

2012 ◽  
Author(s):  
Christine Hansen ◽  
Tom Griffiths
Keyword(s):  
Catchment Area ◽  
National Park ◽  
Human History ◽  
River Catchment ◽  
The Past ◽  
Historical Archives ◽  
History Of ◽  
Shallow Basin ◽  
The Relationship ◽  
Yarra River

Within the Yarra River catchment area nestles the valley of Steels Creek, a small shallow basin in the lee of Kinglake plateau and the Great Dividing Range. The escarpment walls of the range drop in a series of ridges to the valley and form the south-eastern boundary of the Kinglake National Park. The gentle undulations that flow out from the valley stretch into the productive and picturesque landscape of Victoria’s famous wine growing district, the Yarra Valley. Late on the afternoon of 7 February 2009, the day that came to be known as Black Saturday, the Kinglake plateau carried a massive conflagration down the fringing ranges into the Steels Creek community. Ten people perished and 67 dwellings were razed in the firestorm. In the wake of the fires, the devastated residents of the valley began the long task of grieving, repairing, rebuilding or moving on while redefining themselves and their community. In Living with Fire, historians Tom Griffiths and Christine Hansen trace both the history of fire in the region and the human history of the Steels Creek valley in a series of essays which examine the relationship between people and place. These essays are interspersed with four interludes compiled from material produced by the community. In the immediate aftermath of the fire many people sought to express their grief, shock, sadness and relief in artwork. Some painted or wrote poetry, while others collected the burnt remains of past treasures from which they made new objects. These expressions, supplemented by historical archives and the essays they stand beside, offer a sensory and holistic window into the community’s contemporary and historical experiences. A deeply moving book, Living with Fire brings to life the stories of one community’s experience with fire, offering a way to understand the past, and in doing so, prepare for the future.

scholarly journals Silicon in ultrafresh groundwater: a case study of the Imandra Lake catchment, The Kola Peninsula

2019 ◽  
Vol 98 ◽  
pp. 01018
Author(s):  
Natalia V. Guseva ◽  
Yuliya G. Kopylova ◽  
Daria A Vorobeva ◽  
Albina A. Khvashchevskaya ◽  
Zinaida A. Evtyugina
Keyword(s):  
Kola Peninsula ◽  
Catchment Area ◽  
Water Exchange ◽  
Rock Interaction ◽  
Silicon Oxides ◽  
Short Period ◽  
Lake Catchment ◽  
Imandra Lake ◽  
Water Rock Interaction

The ultrafresh groundwater (with TDS values less than 200 mg/L) of the Imandra Lake catchment, Kola Peninsula, is from an intensive water exchange zone, where the water has a short period of contact with the rock. Therefore, the considered water is at the initial stages of the water–rock interaction. The water is saturated with respect to oxides and hydroxides of aluminium and iron. In the groundwater of the Imandra Lake catchment area, the silicon concentrations significantly exceed the concentrations of magnesium and especially potassium. Nevertheless, water is undersaturated with respect to with respect to silicon oxides. The shown enrichment of water with cations is explained by time of water-rock interaction.

scholarly journals The Ecology of Rawa Aopa, a Peat-swamp in Sulawesi, Indonesia

1992 ◽  
Vol 19 (3) ◽  
pp. 226-234 ◽  
Author(s):  
Robert Zwahlen
Keyword(s):  
Catchment Area ◽  
National Park ◽  
Human Population ◽  
Water Regime ◽  
Point Of View ◽  
Tourist Attraction ◽  
Sustainable Utilization ◽  
Peat Swamp ◽  
Food Fish ◽  
Primary Forests

Rawa Aopa is a large swamp in South-East Sulawesi, Indonesia — the only major peat-swamp in this mainly mountainous island. Its vegetation and fauna are still quite poorly known. The existing information is summarized here. With the creation of new villages as part of Indonesia's transmigration programme, the human population in this area has increased very rapidly. Pressure on natural resources — especially soils and forests — is increasing, and primary forests are dwindling rapidly. This in turn increases the threats to Rawa Aopa, as erosion in its catchment area inevitably leads to a rapid silting up of the swamp. The swamp has a potential as a source of food (fish and sago) and income (rattan and other products), and it might to some degree become a tourist attraction.From a scientific point of view, the gaps in the knowledge about water-regime, vegetation, and fauna, ought to be remedied. In order to attain sustainable utilization of this area, a thorough plan ought to be made for the whole catchment of Rawa Aopa. The most important measure to take is the protection of the forests covering the hills and the surroundings of the swamp. Also important very widely is the protection of soils. Furthermore, it is recommended to include the northern part of the swamp in the already-existing Rawa Aopa—Watumohai National Park.

scholarly journals Estimation of soil erosion and sediment yield concentration across the Kolleru Lake catchment using GIS

2021 ◽  
Vol 80 (4) ◽  
Author(s):  
Meena Kumari Kolli ◽  
Christian Opp ◽  
Michael Groll
Keyword(s):  
Land Use ◽  
Soil Erosion ◽  
Soil Texture ◽  
Sediment Yield ◽  
Soil Loss ◽  
Catchment Area ◽  
Drainage System ◽  
Delivery Ratio ◽  
Lake Basin ◽  
Lake Catchment

AbstractFlat lakes with a large catchment area are especially affected by sediment inputs. The Kolleru Lake catchment (south-eastern India) with a surface area of approximately 6121 km2 belongs to such types of lake basins. The study’s main objective was the assessment of both soil erosion and sediment yield concentration rate of the Kolleru catchment. The study was conducted using the revised universal soil loss equation (RUSLE) model due to its simple and good applicability for soil erosion estimation. Data such as rainfall, soil texture, topography, crop cover management, and support practice factor were integrated into the modeling using RUSLE and ArcGIS. Field data were used both to analyze the soil texture and the slope length factor. The results showed that average annual soil loss was estimated with 13.6 t/ha/year, classifying the Kolleru Lake Basin under a very high erosion rate category. About 38% of the catchment area has encountered slight soil loss. Areas covered with moderate, strong, severe, very severe erosion potential zones are 29%, 17%, 9%, and 5.5%, respectively. This study identified that upland areas with less vegetation cover exported high potential erosion rates. Unlike the soil loss, the sediment delivery ratio values for the catchment were not affected by land use, while it showed a strong relationship with the catchment drainage system. Whereas, the average annual sediment yield was determined with 7.61 t/ha/year, had identified with the same pattern of the soil erosion. Catchment topography, vegetation, drainage system, soil properties, and land use cover played a major role in exporting the highest sedimentation. The outcome of these studies can be used among others to identify critical erosion areas on a pixel basis for the planning of erosion management practices.

scholarly journals Does glacial retreat impact benthic chironomid communities? A case study from Rocky Mountain National Park, Colorado

2021 ◽  
Vol 3 (12) ◽  
Author(s):  
Danielle R. Haskett Jennings
Keyword(s):  
Surface Water ◽  
Water Temperature ◽  
National Park ◽  
Rocky Mountain ◽  
Environmental Variable ◽  
Rocky Mountain National Park ◽  
Surface Water Temperature ◽  
Running Water ◽  
Glacial Meltwater ◽  
Lake Catchment

AbstractThe aim of this study was to determine which environmental variables are responsible for modern benthic chironomid distributions in a glacial setting. The chironomid communities from nine alpine lakes were assessed, and forty-three individual taxa were extracted and identified. Surface water temperature and nitrate were strongly and negatively correlated (−0.82, p = 0.007), suggesting that glacial meltwater (the driver that explains both surface water temperature (SWT) (°C) and nitrate (NO3 + NO2-N)) is the environmental variable that explains the most variance (15%). On average, lakes receiving glacial meltwater were 2.62 °C colder and contained 66% more NO3 + NO2-N than lakes only receiving meltwater from snow. The presence of taxa from the tribe Diamesinae indicates very cold input from running water, and these taxa may be used as a qualitative indicator species for the existence of glacial meltwater within a lake catchment. Heterotrissocladius, Diamesa spp., and Pseudodiamesa were present in the coldest lakes. Chironomus, Diplocladius, and Protanypus were assemblages found in cold lakes affiliated with the littoral zone or alpine streams. The modern benthic chironomid communities collected from the alpine of subalpine lakes of Rocky Mountain National Park, Colorado, represent a range of climatic and trophic influences and capture the transition from cold oligotrophic lakes to warmer and eutrophic conditions.

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