The research shows the analysis and characteristics of potential hydrological windows in Cracow against the background of the environmental characteristics of the city and the expected profits from the use of areas of the decommissioned industry. The authors, additionally, based on the optimal species of vegetation, indicated possible methods of using individual species.
2.1. Environmental and Climatic Conditions Related to the Location of Cracow
Cracow is known in the world primarily for its centuries-old heritage, inscribed in the fabric of the city. However, it was also an industrial center, the beginnings of which date back to the 19th century, the industrial revolution and the location of enterprises such as: Zieleniewski, Piasecki and Peterseim in Cracow. The post-war period made it a very important industrial center of Poland and the center of the Cracow Industrial District, which included smaller towns located today in the metropolitan area—primarily: Bochnia, Myślenice, Skawina, Wieliczka, Trzebinia, Chrzanów and Olkusz. Cracow specialized mainly in the metallurgical industry and related functions, but not only. The flagship investment of that time was Lenin’s ironworks (Huta im. Lenin) launched on 22 July 1954.
The city is located on the lower border of the moderately warm climate of Karpat, as a type of basin climate. It is characterized by a wide variety of weather conditions, resulting from the influx of various air masses to this area, mainly polar-sea, causing thaws and precipitation in winter, and cooling, precipitation and storms in summer, and to a lesser extent: warm tropical-sea throughout the year. or continental, as well as always cool and dry Arctic air. The city’s climate, compared to non-urban areas, is distinguished by, inter alia, higher air temperature, lower values of relative humidity and a greater number of dry days, fewer days with fog, more days with a storm, weaker solar radiation intensity, lower wind speeds, shorter dependence—snow cover or greater air pollution [
9].
The most characteristic feature of the city’s climate is the presence of higher air temperature values in the center of the agglomeration than in its outskirts. This phenomenon is known as the urban heat island. The influence of the city on the air temperature is more pronounced in the case of its minimum values, rather than the maximum ones. The average annual air temperature for Cracow is 8.8 °C (
Table 1). In Cracow, annual precipitation totals most often reach values in the range of 650–730 mm, and the average annual rainfall is 688 mm [
10]. Precipitation of this type, genetically related to the flow of air from the northern quadrant, is the most common cause of flooding in the upper Vistula basin. All this is related to the location of cities in the floodplains of the Vistula River (
Figure 2). Many of the current limitations in the city’s development and environmental conditions, such as areas of stagnant fogs or easily formed smog, result from the original location of the city in the area of the Vistula overflow.
On the one hand, swamps and wetlands are a factor limiting the city’s development, and at the same time they are very important areas for natural water retention. They are particularly valuable components of the natural system due to their role in shaping the microclimate as well as aesthetic and recreational values. They are the mainstay of many important and valuable flora and fauna communities. Over the years, along with the development of the city, they underwent a transformation, often leading to a complete disappearance. Despite this, there are still many wetlands in Cracow, which constitute valuable natural and landscape enclaves. The amount of rainfall from June to August (the maximum rainfall occurs in July) is almost three times higher than in the winter season, which proves a large degree of pluvial continentalism in Cracow.
Precipitation in Cracow occurs on average 173 days a year. In the center of Cracow, on average, there are about 30 days with a storm every year [
11]. These values in combination with the increasing density of the urban tissue cause a conflict between the natural conditions of the environment and human activity, which is in conflict with the balancing of the city’s development. Miejskie Przedsiębiorstwo Wodociągów i Kanalizacji S.A. (MPWiK S.A., Warshaw, Poland) states that the sewage system of Cracow is solved in a combined system in the central parts of the city and a distribution system on its outskirts, in the vicinity of rivers. The peripheral areas of Cracow are intended for sewerage in local systems. The city still has deficiencies in the technical infrastructure, mainly in the collection and treatment of wastewater and rainwater, and in water supply. These deficiencies occur mainly on the outskirts, in the so-called “peripheral areas” of Cracow. The growing problem of rainwater management remains to be solved in areas where there is intensive investment.
There are potentially many reasons for this state of affairs (infrastructural, financial and awareness shortages), but it is worth focusing on the possibilities of its improvement.
2.2. Green Areas in Post-Industrial Areas—Changes in Industrial Structures and Green Areas in the Last 50 Years
In the Polish reality, changes in infrastructure to improve municipal water management take place slowly. This is combined with changes in land use in the changing image of the city. The importance of integrated urban landscape planning for the management of water resources seems to be extremely important. In particular, it is necessary to emphasize the importance of biologically active hydrological windows with bioretention functions that may arise in post-industrial areas, replacing the operation of technical devices with their operation. Due to the history of these places, it would be important to preserve the memory of their former function and to leave some post-industrial relics in an ecologically active landscape [
12]. The areas of hydrological windows can be included in a network of green-blue infrastructure [
13], because in this area there will be bioreactive basins, artificial wetlands, mineral and plant filters—used in biologically active water reservoirs. The changes in the city’s structure are incremental and are related to development pressure and insufficient legal protection. In recent years, the investment pressure in Cracow has resulted in a fourfold increase in employment in service and business areas. It grows every year, causing changes in the city space. In Cracow, there was a definitive collapse of industry and with it the liquidation of jobs. Today, the expectations of the post-industrial society are different. We want to live in an ever cleaner environment. We stop producing there, generating and processing information. Housing and office estates are built on the site of former factories, warehouses and enterprises. Industrial facilities are disappearing from the city structure and replaced by office buildings of international corporations. “Fabryka Zieleniewskiego” (Zakłady Budowy Maszyn i Aparatury im. L. Zieleniewski S.A. (
Table 2), Cracow, Poland) has given way to blocks of flats, and the “Polmos” alcoholic beverages factory has also disappeared. The same happened with the Artigraph factory at ul. Prądnicka, as well as the service area, the Peterseima factory at ul. Zółkiewski.
When analyzing the areas of decommissioned industry over the last half-century, it should be noted that they are dispersed against the city’s buildings (
Figure 3). If only the potential of these areas were used as such that enable the retention of rainwater and snowmelt, Cracow would have a much better microclimate, a more coherent network of green and blue infrastructure and lower loads of water discharge into the sewage system. Unfortunately, this did not happen and only 3 larger areas gained biologically active functions. The first is the Zakrzówek limestone quarry. The closed excavation (1992) was reclaimed by flooding it with water. Currently, ecologists are fighting for the species protection of the blue tit and smooth snake, which makes it easier to keep it and its surroundings as a green area. The Regional Directorate for Environmental Protection is working on including this area and its buffer zone [
14]. A small quarry-meme in nature protection (inanimate nature reserve) is also a marl mining quarry called Bonarka (until 1961).
Another area, also post-mining, is the area of the limestone quarry called Lebanon (named after the owner). The quarry area was excluded from production in 1986. Others, of which there were 7 more in this location, were closed, as was Lebanon by 1986 [
15]. The Liban quarry is also subject to vegetation succession, and its bloody history (it was a labor camp established by the Nazis during the occupation of Cracow in 1942) prevented any attempts to urbanize it.
Most of the brownfield sites failed to withstand the investment pressure [
16,
17]. Most of them have been densely built-up, preventing free water filtration. Industrial areas that still perform technical functions include the municipal heating plant MPEC SA, located in the area between Cracow and the Nowa Huta district, close to the river. It is an industrial and communal function, the purpose of which is not threatened by any changes so far, and the area is used extensively, giving place to the green structure.
The production area (or actually in 2021 already post-production) is the former metallurgical plant (originally the Lenin Steelworks, until 1990, and then T. Sędzimir until 2004 and now Acellormittal) for which a whole residential district was built. The area of the smelter was combined with the areas to the south of it, which served as auxiliary waste dumps, treatment plants, settling tanks, etc. The area is adjacent to the immediate vicinity of the Vistula River and its vegetation is degraded as a result of industrial use.
These areas and other larger post-industrial areas are located in the river valley and in the oxbow lake of the Vistula. The direction of their transformation and hydrological protection are all the more important. Most of these areas have native vegetation of a bioretical nature characteristic of wetlands.
Plant species occurring in the area of the Vistula valley in its upper course—for rainwater management under bioretention, based on [
18] (
Table 3).
The substrate is also important in the entire bioretention system [
19]. It is in the Vistula valley at the beginning of the Carpathian Foredeep that it seems naturally adapted. The use of a bioretention system requires min. about 5% of the ground area of the area from which rainwater is collected, therefore the best candidates for their application are hydro-electric windows with free peripheral areas, parking lots and large buildings. The areas where the existing solutions for draining rainwater require modernization are particularly suitable for the introduction of a bioretention system. In the areas subject to bioretention, an important factor enabling water retention are various types of land depressions, basins, water reservoirs rich in water-loving vegetation. Management of surface runoff is carried out in the areas of bioretention in 4 zones (
Table 4).
Each of these zones has a bioretention function and also purifies the aquatic environment. Of course, it is impossible to list all potential plants in all zones, so the table above presents the most popular for southern Poland and the river valleys located in it (
Table 5).
The development of appropriate plant species supports the processes of biological decomposition of organic matter and leads to periodic bioaccumulation of nitrogen and phosphorus in plant tissues. As shown by studies in plant tissues, 5–10% of the load supplied to the nitrogen system can be periodically retained. The amount of bioaccumulated nitrogen depends both on the type of plants and their growth phase. You can see the multi-layered benefits of using bioretention here.