Historical medium-scale maps as a source of information on the overgrowing of lakes

In the work, medium-scale topographic maps from the first half of the 20th century and aerial photographs from the first decade of the 21st century were used to determine the rate of overgrowing of lakes. A comparison of results for lakes located in different parts of Poland demonstrated that the pr...

Full description

Bibliographic Details
Main Author: Ptak Mariusz
Format: Article
Language:English
Published: Sciendo 2013-09-01
Series:Limnological Review
Subjects:
Online Access:https://doi.org/10.2478/limre-2013-0017
id doaj-a97878a561b04356979f43d7c1d68f0a
record_format Article
spelling doaj-a97878a561b04356979f43d7c1d68f0a2021-09-06T19:22:23ZengSciendoLimnological Review2300-75752013-09-0113315516210.2478/limre-2013-0017Historical medium-scale maps as a source of information on the overgrowing of lakesPtak Mariusz0Department of Hydrology and Water Management, Institute of Physical Geography and Environmental Planning, Adam Mickiewicz University, Dzięgielowa 27, 61-680 Poznań, PolandIn the work, medium-scale topographic maps from the first half of the 20th century and aerial photographs from the first decade of the 21st century were used to determine the rate of overgrowing of lakes. A comparison of results for lakes located in different parts of Poland demonstrated that the process of proliferation of emergent plants dominated - such a situation was recorded for 14 out of the 15 lakes analysed in the work. The calculated average overgrowing rate for all the lakes in the years 1945-2010 was 0.4 ha yr-1. Lake Karaś (1.83 ha yr-1) and Lake Oświn (1.2 ha yr-1) were characterized by the highest overgrowing rates. Moreover, the work presents an attempt at discovering the factors which determine the scale of the lake overgrowing process. To this end, the main lake parameters were analysed and it was concluded that the rate of overgrowing of lakes was influenced, inter alia, by water level fluctuations and the shape and depth of a given lake. However, each lake should be treated as an individual object which responds to the processes occurring in its environment in a unique way.https://doi.org/10.2478/limre-2013-0017overgrowingmacrophytes successionlakeshistorical maps
collection DOAJ
language English
format Article
sources DOAJ
author Ptak Mariusz
spellingShingle Ptak Mariusz
Historical medium-scale maps as a source of information on the overgrowing of lakes
Limnological Review
overgrowing
macrophytes succession
lakes
historical maps
author_facet Ptak Mariusz
author_sort Ptak Mariusz
title Historical medium-scale maps as a source of information on the overgrowing of lakes
title_short Historical medium-scale maps as a source of information on the overgrowing of lakes
title_full Historical medium-scale maps as a source of information on the overgrowing of lakes
title_fullStr Historical medium-scale maps as a source of information on the overgrowing of lakes
title_full_unstemmed Historical medium-scale maps as a source of information on the overgrowing of lakes
title_sort historical medium-scale maps as a source of information on the overgrowing of lakes
publisher Sciendo
series Limnological Review
issn 2300-7575
publishDate 2013-09-01
description In the work, medium-scale topographic maps from the first half of the 20th century and aerial photographs from the first decade of the 21st century were used to determine the rate of overgrowing of lakes. A comparison of results for lakes located in different parts of Poland demonstrated that the process of proliferation of emergent plants dominated - such a situation was recorded for 14 out of the 15 lakes analysed in the work. The calculated average overgrowing rate for all the lakes in the years 1945-2010 was 0.4 ha yr-1. Lake Karaś (1.83 ha yr-1) and Lake Oświn (1.2 ha yr-1) were characterized by the highest overgrowing rates. Moreover, the work presents an attempt at discovering the factors which determine the scale of the lake overgrowing process. To this end, the main lake parameters were analysed and it was concluded that the rate of overgrowing of lakes was influenced, inter alia, by water level fluctuations and the shape and depth of a given lake. However, each lake should be treated as an individual object which responds to the processes occurring in its environment in a unique way.
topic overgrowing
macrophytes succession
lakes
historical maps
url https://doi.org/10.2478/limre-2013-0017
work_keys_str_mv AT ptakmariusz historicalmediumscalemapsasasourceofinformationontheovergrowingoflakes
_version_ 1717772286177574912