Post-mining Sites Research Articles

The role of civic engagement in post-mining environmental revitalization

Abstract The large tin potential in the Bangka Belitung Islands has an impact on the high level of mining activity that has been carried out for a long time. The ecological impact of mining activities leaves behind post-mining pits or known as kulong are not properly reclaimed. Large and spacious kulongs are found in Perlang and Nibung Villages, Central Bangka Regency. This research explains the contribution of local community towards tourism awareness groups “Pokdarwis” and village-owned enterprises “Bumdes” in revitalizing post-mining sites to become tourist destinations known as Lake Pading and Lake Kaolin. Designed as a qualitative-descriptive approach, the data collection was carried out through observation, interviews and document study. Research findings show that the revitalization of post-mining pit areas, specifically at Lake Pading and Lake Kaolin by Pokdarwis and Bumdes has had a significant impact on the escalation of environmental and tourism use values. Efforts to increase tourism are also a means of sustainable environmental preservation and preventing damage from illegal mining activities. Community participation in revitalizing and preserving the environment reflects principles that are in accordance with the concept of Civic Engagement.

Identification of groundwater flow on ex-mining area using the self potential method as an initial stage of post-mining site reclamation at Red Hill, Bangka

Abstract The Red Hill area in Bangka Regency, one of the largest former mining sites on Bangka Island, remains largely unreclaimed, presenting opportunities for sustainable rehabilitation. This study utilizes the Self-Potential (SP) method to map groundwater flow patterns as a foundation for post-mining reclamation efforts. SP data were collected along eight survey lines, covering 150-250 meters each, in the Ampar Lake area. The analysis reveals SP anomalies ranging from -117 mV to 86,696 mV, indicating significant variations in electric potential linked to groundwater movement. High-potential zones were identified as recharge areas, while low-potential zones indicate discharge areas, suggesting a regional groundwater flow from northeast to southwest. These findings establish a preliminary understanding of groundwater behavior in the Red Hill area, providing a basis for targeted reclamation to support agricultural, educational, and ecotourism initiatives.

Water provision benefits from karst ecosystems: An example for Watuputih groundwater basin, North Kendeng Mountain, Indonesia

Karst ecosystems offer a wealth of ecosystem services, but their protection is increasingly challenging due to degradation and land-use conversion, including limestone mining. This study investigates the water provision service derived from karst ecosystems threatened by limestone mining in the Watuputih groundwater basin, Central Java, Indonesia. Water supply was quantified by measuring water discharge rates from major springs around the basin. Water usage was quantified for household consumption, agriculture, and recreation. This study also measured water infiltration rates in mining and non-mining areas to indicate the effects of limestone mining to hydrological processes. This study identified three primary springs around the basin: Sumber Seribu spring, Brubulan spring, and Kalutan spring, with discharge rates of 1080 L per second, 85 L per second, and 0.76 L per second, respectively. A local water company extracts water from Sumber Seribu spring at a rate of 80 L per second to supply approximately 57,600 individuals. The water supply from the three springs can irrigate approximately 1594 ha of rice fields. Water from Sumber Seribu spring also supports recreational activities in Sumber Semen recreation park, attracting an average of 19,173 visitors per year. This study revealed a complete impairment of soil's water infiltration capacity in limestone mining areas. These findings underscore the pressing need to safeguard the Watuputih groundwater basin and to mitigate the detrimental effects of limestone mining on hydrological processes. This involves designating the Watuputih karst ecosystem as a protected area, implementing Payment for Ecosystem Services (PES) programs, and restoring degraded post-mining sites.

How the effect of earthworms on soil organic matter mineralization and stabilization is affected by litter quality and stage of soil development

Globally soil fauna consumes about half of the annual litter fall. An important question is how this activity affects the mineralization and stabilization of soil organic matter. Here we explore how much earthworms influence the decomposition of litter and the stabilization of organic matter in soils at various stages of soil development (various soil age) that are supplied with litter of various quality. The laboratory mesocosms consist of litter and a mineral layer. The mineral soils originated either from spruce and alder stands growing either on post-mining soils (young soils after about 50 years of soil development) or from soils in the close vicinity of post-mining sites (mature soils with several thousand years of soil development), the mineral soils were supplied by matching litter, the mesocosms were either without earthworms or with two individuals of earthworms. The earthworm effect showed statistically significant interaction with tree and soil age: earthworms increased respiration in both alder soils, but in spruce soils only in mature soil, while the opposite was true for young soils. In general, earthworms promoted the removal of litter from the soil surface and carbon accumulation in the mineral soil. Earthworms promoted C storage in mineral associated organic matter (MAOM), especially in young spruce soils. The results suggested that earthworm activity in young soils which were far from saturation (spruce on post-mining soils) promotes soil C sequestration by promoting C storage in MAOM, whereas earthworms in mature, C saturated soils tend to promote soil respiration. More broadly, earthworms effect on soil depends on stage of soil C saturation.

Long-term agricultural reclamation on the chemical properties of Technosols at lignite postmining site – efficiency of winter wheat and winter rape

Long-term agricultural reclamation on the chemical properties of Technosols at lignite postmining site – efficiency of winter wheat and winter rape

Establishment of Nitrogen-Fixing Frankia, Arbuscular Mycorrhizal Fungi, and Their Effects on Alder (Alnus glutinosa L.) Growth in Post-Mining Heap Soils

Planting nitrogen-fixing plants in post-mining sites and similar degraded areas is a common approach to speed up soil development and buildup of the nitrogen pool in soil organic matter. The aim of this study was to explore if slower growth of alder seedlings in initial post-mining sites results from adverse soil conditions or lack of microbial symbionts. To address this question, we sampled young soil (age 15 years) and more developed soil (age 70 years) from heaps after coal mining near Sokolov (Czech Republic). Soil samples were sterilized and not inoculated or inoculated with arbuscular mycorrhizal fungi (AMF) or AMF + Frankia, followed by planting with alder (Alnus glutinosa) seedlings germinated and precultured under sterile conditions. The effect of soil age on alder growth appeared to be non-significant. The only significant growth effect was seen with Frankia inoculation, implicating this inoculum as a key factor in later succession in post-mining soils. When the soil was fully inoculated, alder biomass was higher in developed soil supplied with iron (Fe) and phosphorus (P), indicating that iron and phosphorus availability may affect alder growth. In young soil, alder growth was highest with a combination of iron, phosphorus, and sulfur (S), and a positive effect of sulfur in young soil may correspond with a reduced, alkaline soil pH and increased phosphorus and iron availability.

Visiting mine reclamation: How field experience shapes perceptions of mining

Recognizing the prevailing negative public opinion on mining, it is important to understand how firsthand encounters with mining activities might influence these perceptions. This study investigates how field trips to open pit coal mines and their reclamation sites in the Czech Republic affected the attitudes of 148 university students toward mining and mine reclamation. Using pre and post trip questionnaires, we observed significant changes: Students became less neutral about mining, saw it as a temporary disruptive activity, expressed reduced concern for social conflicts in mining areas, and showed increased support for the ecological restoration of post mining sites. These findings underscore the transformative impact of direct engagement with mine reclamation activities on shaping attitudes. Understanding these effects offers promise for positively shifting public perceptions of mining practices, emphasizing the potential for constructive changes in attitudes through field experiences with reclamation efforts in the Global North.

Spatial estimation of soil organic carbon, total nitrogen, and soil water storage in reclaimed post-mining site based on remote sensing data

The estimation of Soil Organic Carbon (SOC), Total Nitrogen (TN), and Soil Water Storage (SWS) is crucial in comprehending ecosystem services and environmental sustainability. It plays a crucial role in guiding sustainable restoration strategies and supporting the long-term health of post-mining sites. Remote sensing technology provides valuable tools for modelling and mapping soil properties in reclaimed post-mining sites efficiently and cost-effectively. This study aimed to utilize remote sensing data to estimate SOC, TN, and SWS in a reclaimed post-mining site. Field data was collected from 130 research plots to obtain reference data for SOC, TN, and SWS from the Sonica hard coal post-mine spoil heap. Remote sensing data were: airborne laser scanning (ALS) point clouds and Planets cope satellite imageries. Generalized Additive Models (GAM) were used to develop predictive models. Wall-to-wall predictions of analyzed variables were performed. The results identified topographic and remote sensing indicators that significantly influence SOC, TN, and SWS. Digital Terrain Model (DTM), aspect, and blue spectral band are variables that explain SOC storage, with a significant influence of DTM, ranging from −8 to 18 Mg ha−1. TN was explained by DTM, Canopy Height Model (CHM), blue and Near Infrared (NIR) spectral bands, and Normalized Difference Vegetation Index (NDVI), mainly influenced by NIR and NDVI, ranging from −1.1 to 0.8 and −0.9 to 1.4 Mg ha−1, respectively. The values of Topographic Wetness Index (TWI), aspect, CHM, blue and NIR spectral bands explained SWS, highlighting their importance in assessing soil water dynamics in post-mining landscapes, with TWI and CHM being particularly influential, ranging from −2 to 5.1 and −6 to 2 mm, respectively. However, caution is advised when predicting SOC and TN using remote sensing in post-mining sites due to geogenic carbon considerations.

Biodiversity Characteristics and Carbon Sequestration Potential of Successional Woody Plants Versus Tree Plantation under Different Reclamation Treatments on Hard-Coal Mine Heaps––A Case Study from Upper Silesia

In the discussion about sustainable forestry, a key role is played by the development of ecosystem services, including ecological, social, and economic ones, in which biodiversity and carbon (C) sequestration are among the most important. Afforestation of disturbed and post-mining sites is one of the ways to minimize the negative impact of civilization on the environment. Optimizing C sequestration strategies at post-mining sites plays a crucial role in promoting ecosystem recovery, supporting climate change mitigation, and enabling C offsetting. In this study, we compared the C storage in the soil and plant biomass of forest ecosystems developed on coal-mine heaps for different scenarios of reclamation and succession. We tested combinations of sites (i.e., non-reclaimed sites on bare carboniferous rock [BR] and sites reclaimed by applying topsoil [TS]) and successional woodland and tree plantation. The estimated potential for total C storage (in the soil + biomass) for TS sites ranged from 68.13 to 121.08 Mg ha−1, of which 52.20–102.89 Mg ha−1 was stored in the soil and 12.09–20.15 Mg ha−1 in the biomass. In the non-reclaimed sites on BR, the total C storage was much higher, amounting to 523.14 Mg ha−1 (507.66 Mg ha−1 being in the soil), which was due to the geogenic coal content in the BR. However, the C storage in the biomass (15.48 Mg ha−1) and litter (5.91 Mg ha−1) was similar to the amounts obtained from the reclaimed sites. The number of species did not differ statistically significantly between the analyzed variants. On average, 14 species were recorded in the plots. The average Shannon–Wiener index (H’) value was higher for sites with BR (1.99) than TS variants on reclaimed plots (1.71). The lowest H’ value was for those plots with Robinia pseudacacia in the stand. One of the main implications of the obtained results for sustainable forestry is the perspective of using succession in the recovery of a disturbed ecosystem. We noted that woodlands from succession on BR are highly biodiverse, have high C sequestration potential, and do not require time-consuming reclamation treatments.

Mucor thermorhizoides—A New Species from Post-mining Site in Sudety Mountains (Poland)

Mucor representatives are mostly rapidly growing cosmopolitan soil saprotrophs of early diverged Mucoromycotina subphylum. Although this is the most speciose genus within the group, some lineages are still understudied. In this study, new species of Mucor was isolated from the post-mining area in southwestern Poland, where soil chemical composition analysis revealed high concentration of hydrocarbons and heavy metals. Phylogenetic analysis based on multigene phylogeny showed that the new isolate clusters distinctly from other Mucor species as a sister group to Mucor microsporus. New species Mucor thermorhizoides Abramczyk (Mucorales, Mucoromycota) is characterized by the extensive rhizoid production in elevated temperatures and formation of two layers of sporangiophores. It also significantly differs from M. microsporus in the shape of spores and the size of sporangia. M. thermorhizoides was shown to be able to grow in oligotrophic conditions at low temperatures. Together with M. microsporus they represent understudied and highly variable lineage of the Mucor genus.

Solution for Post-Mining Sites: Thermo-Economic Analysis of a Large-Scale Integrated Energy Storage System

The intensive development of renewable energy sources and the decreasing efficiency of conventional energy sources are reducing the flexibility of the electric power system. It becomes necessary to develop energy storage systems that allow reducing the differences between generation and energy demand. This article presents a multivariant analysis of an adiabatic compressed air energy storage system. The system uses a post-mining shaft as a reservoir of compressed air and also as a location for the development of a heat storage tank. Consideration was given to the length of the discharge stage, which directly affects the capital expenditure and operating schedule of the system. The basis for the analyses was the in-house numerical model, which takes into account the variability of air parameters during system operation. The numerical model also includes calculations of Thermal Energy Storage’s transient performance. The energy efficiency of the system operating on a daily cycle varies from 67.9% to 70.3%. Various mechanisms for economic support of energy storage systems were analyzed. The levelized cost of storage varies, depending on the variant, from 75.86 EUR/MWh for the most favorable case to 223.24 EUR/MWh for the least favorable case.

Two new species of Achaeta (Enchytraeidae, Oligochaeta) from afforested post-mining and post-fire sites in Poland.

Achaeta (Enchytraeidae, Oligochaeta, Clitellata) is a genus of small, soil-dwelling annelids, peculiar by the absence of chaetae in all species. Here two new species of this genus are described from afforestation sites in southern Poland. Descriptions are based on the investigation of living and preserved material. The species are also characterized at the DNA level, using fragments of the COI and ITS genes, sequenced from the holotypes and paratypes. The worms are not longer than 4-6 mm, with about 30 to 35 segments, and with medium-large male and female reproductive organs. Achaeta florens sp. nov., discovered at a post-mining site, has four segmental pyriform glands, an oesophageal appendage restricted to segment V, a clitellum with distinct transverse rows and dorsal and ventral interruption, and spermathecae with blossom-like fields of vesicular gland cell apices around the ventrally located ectal pores. The species is without peculiar characters but the combination of characters is diagnostic. Its morphological distinction from A. nurmineni, described from the Indian subcontinent, is difficult due to the poor description of that species; A. nurmineni is therefore considered a species inquirenda. Achaeta gemmata sp. nov., discovered in high abundance at a post-fire site, is without pyriform glands but with conspicuous, gem-like lateral papillae in all preclitellar segments. The papillae are modified and enlarged epidermal gland cells that protrude into the body cavity. The species is without oesophageal appendage and has a dorsally closed clitellum and lateral spermathecal pores. It is superficially similar to Achaeta camerani, found at the same site, but can be distinguished based on sexual and non-sexual characters. A comparison of COI sequences showed 100% identity with a specimen from Sweden, erroneously identified as A. cf. brevivasa. Genetic distance between the two new species based on COI differences is 20%, distances to other species of Achaeta with publicly available COI sequences range from 16% to 26%.

Stable isotope insights into arthropod food chains and nitrogen cycling in a rehabilitated tailings chronosequence

Field studies in post-mining sites on epigeic invertebrate groups are scarce despite their importance in pedogenesis and ecosystem multifunctionality. This research investigated the diversity, abundance and succession of aboveground invertebrates in a rehabilitated Pb/Zn tailings chronosequence of 5, 20 and 35 years. The study also explored the trophic relationship of selected arthropods and characterized the nitrogen (N) cycle using stable isotope measurements. The abundance and species richness in most investigated groups and the dominance index Berger–Parker (BP) of aboveground invertebrates increased with rehabilitation age from 0.17 BP in early to 0.31 BP in late stage. Elemental and stable isotope ratio analysis showed that N and C soil content increased and the C/N ratio decreased with age, yet despite this increased N availability in the system, the maturing N-cycle used N efficiently. The lack of large N losses from the system despite substantial atmospheric deposition inputs was indicated by the fact that N isotope ratios (δ15N) in plants and animals became significantly more negative with rehabilitation age, −6.0 δ15N for plants, −5.0 δ15N for herbivores and 3.0 δ15N for carnivores. The length of the invertebrate food chain expanded by more than half a trophic level (2.7‰ δ15N) for top predator Coleoptera from early to late stage, probably reflecting more complex food webs including intra-guild predation in older communities. In conclusion, δ15N measurements in plants and animals provided novel insights into the N-cycle, accumulative N flows and the trophic position in post-mining sites. It is proposed that isotope ratio measurements could be used as easy-to-measure, integrating indicators of nutrient cycling and the soil food web complexity of rehabilitated mine tailings and similar soil ecosystems.

Metody rewitalizacji obszarów pokopalnianych na przykładzie światowych realizacji architektonicznych i studiów własnych

Post-mining grounds and spoil tips frequently render landscapes permanently flawed. As a result of mining activity, considerable stretches of land are often permanently excluded from further use. Due to the extensively transformed landscape, it is necessary to implement revitalisation processes. Relevant design and investment activities, coupled with the cooperation of specialists such as architects, civil engineers, geotechnicians, hydrotechnicians and environmental engineers, along with local authorities, can offer a comprehensive functional programme for areas degraded by mining and provide local residents with an attractive leisure area. This article discusses the current state of knowledge on the revitalisation of former mining areas, with special regard to architectural, environmental, social, and economic aspects. The aim of the study is to review and promote design solutions which permanently restore previously degraded areas to local communities. Various concepts of revitalisation of degraded areas are presented, based on examples of landscape architecture at home and abroad. The selected examples comprise natural regeneration, reclamation, and ecological engineering. These are examples of a holistic and modern approach to the development of tourist and environmentally active areas in post-mining sites and spoil tips. Furthermore, the study presents the authors' proposal concerning the revitalisation of a spoil tip area at LW Bogdanka mine for winter sport purposes and other activities, for which the demand was signalled by their management. The discussed examples can serve as an inspiration for future actions and executive projects, undertaken in accordance with the guidelines of Agenda 2030 and Fit for 55 policies.

A game theoretic decision-making approach to reduce mine closure risks throughout the mine-life cycle

ABSTRACT To align a post-mining site to the wants and needs of local communities and stakeholders, mine closure needs to consider criteria which may be difficult to value using conventional cost–benefit analysis. For example, criteria associated with the environment, socio-environmental relationships, health, and long-term sustainability. Game theory techniques are implemented to investigate how different stakeholder groups could act during mine closure planning and decision-making. Using game theory with sustainability criteria, this study proposes an innovative approach to analyze some key decisions throughout the mine life that affect closure. Non-cooperative game theory models are investigated by developing Nash equilibrium equations which are based on the change in environmental risk, economic potential, and impacts on company reputation. The modified equilibrium formulas can highlight the key sustainability criteria for multi-stakeholder closure planning and complex decision-making. The discussion explores how the developed model can assist mining stakeholders in understanding their position during the mine closure process. In all, the game theory and multiple criteria models can help structure and manage the complex closure risks throughout the mine life cycle.

Dianthus sylvestris subsp. sylvestris as a promising candidate for phytostabilization of copper-contaminated post-mining sites in Alpine ecosystems.

The lack of remediation of inactive mine sites is a serious global concern, as they pose risks to the environment, human health, and safety. The potential of Dianthus sylvestris subsp. sylvestris to remediate post-mining sites contaminated with copper (Cu) at high altitudes, which is a challenging task for most management strategies, was explored in this study. More than 1300 mg Cu kg-1 in shoots were found in plants collected at the Monte Avanza legacy mine site (Alps). However, it is unclear whether this is due to hyperaccumulation or foliar contamination. To address this gap, field samples were washed with two different protocols, and a controlled Cu-tolerance test was conducted. While very high Cu concentrations, exceeding the Cu hyperaccumulation threshold of 300 mg kg-1, were found in samples washed with water, results for the plants cleaned with a more rigorous approach with EDTA suggested Cu exclusion strategy. Under controlled conditions, the plant showed Cu hypertolerance but did not hyperaccumulate Cu. Thus D. sylvestris presents a Cu exclusion strategy rather than hyperaccumulation potential, making it a suitable candidate for Cu phytostabilization at high altitude legacy mine sites. The study emphasizes the need for experiments under controlled conditions when assessing the phytoremediation potential.

Carbon sequestration and soil nitrogen enrichment in Robinia pseudoacacia L. post-mining restoration plantations

Robinia pseudoacacia L. (black locust) has been extensively used for restoring degraded lands, following anthropogenic interventions like coal mining. Here we have addressed the contribution of black locust restoration plantations, established on overburden post-mining material, to carbon storage and to soil nitrogen enrichment at the largest lignite center in Greece. Carbon stocks and fluxes in all pools of the ecosystem, as well as the foliar nitrogen resorption efficiency and soil N stocks were quantified and the effect of plantations’ age was tested. The young age of the plantations (4–24 years) resulted in a relatively low total ecosystem C stock (56.7 t ha−1), which was partitioned among the different pools in the following order: above-ground biomass (50%) > black locust-derived SOC (24%) > coarse roots (14%) > deadwood (6%) > forest floor (5%) > fine roots (less than 1%). Litterfall started early in the growing season and together with fine roots that had a turnover rate of 0.62 yr−1, fueled soil organic carbon. SOC accrual, referring to the accumulation of SOC derived by black locust, declined with age. However, further SOC accumulation is expected, based on the potential SOC storage capacity of soil at the area. C stocks in above- and below-ground biomass increased linearly with age. The same response was observed for soil N stock and NRE, indicating that despite the N2-fixing capacity of black locust, there was still a poor pedospheric N supply and a need for efficient N cycling. Overall, the studied restoration plantations have a considerable contribution to C and N accumulation at the degraded post-mining sites. These positive effects are expected to further increase at least until the plantations reach maturity.

Reclamation and revitalization of post-mining sites – ups and downs

During the post-mining activities, all the forms of environment degradation are observed. This article refers to the projects of reclamation and revitalization of post-mining sites. The method of studying reclamation project documents was used to evaluate remedial actions. This allows for a comparative analysis of the obtained effects (the analyzed case) with the planned procedures. It has been shown what the main effects of degradation are caused by surface and underground mining, as well as what procedures are in force for the repair processes (recultivation and revitalization).

Lessons from patch dynamics for ecology and restoration: The succulent Karoo, Sandveld example

A series of long-term field and glasshouse experiments were conducted in the semi-arid Sandveld Bioregion of southern Africa, across a wide range of post-mining site and soil conditions, on the two major plant groups, leaf-succulent shrubs (LSS, which establish in open micro-habitats) and non-succulent shrubs (NSS, which establish in sheltered micro-habitats). Seeding experiments applied a sequential ecological framework intended to reduce the impact of impeding natural ecological processes whilst incorporating processes that facilitate plant establishment. Experimental plots were scaled to naturally operating ecological dynamics at the patch scale, and various potentially facilitative types of shelter and soil amelioration, tested separately. Results are reported over three or six year periods and from four or seven field sites. Shelter generally had a greater effect on plant establishment than soil ameliorants, but this could be either positive or negative, and varied for the two plant groups: LSS establishment was inhibited or neutral under all forms of shelter, NSS were facilitated by types of artificial shelter that could be removed or biodegraded without impacting young plants. Both groups were strongly inhibited under transplanted nurse plants. Water absorbing gels improved LSS establishment but other soil ameliorants had no effect, while milled kelp or nutrients improved NSS establishment (measured as a biomass index or plant abundance, respectively). Finally, site had a greater effect than either shelter or soil ameliorants, and could not be related to any soil or other factors measured, supporting recent studies that explicitly quantify the substantial unknown effects of site and year. Specific recommendations are made for comprehensive, seed-based, nucleated restoration designs for the Sandveld and similar bioregions, while the over-arching results are of universal import to dryland restoration and ecology.

Woody species succession and spontaneous forest development in post-mining sites after coal mining in the Czech Republic

There is little information about long-term spontaneous forest development after industrial disturbances. A field study was done along the chronosequence of unreclaimed post-mining sites (12, 25, 32, 60 and 90 years old), developing by spontaneous succession in the northwestern Czech Republic. Initial stages of forest development (12- to 60-yr-old) were dominated mainly by silver birch (Betula pendula) goat willow (Salix caprea) and aspen (Populus tremula), Norway spruce (Picea abies) also established naturally in the intermediate stages of succession. A 90-yr-old site was close to the expected climax forest with 21 woody species dominated by European oak (Quercus robus L.), supplemented by beech (Fagus sylvatica). The youngest and oldest sites were more diverse and richer sites in woody species than others, as expressed by the Shannon-Weiner and Simpson indices. Conversely, spatial heterogeneity (aggregation) increased with increasing age; however, it became lower at the age of 90 years. Woody species in the understory were more diverse than in the tree layer. Overall, our study found that spontaneous processes can lead to the development of the late-successional forest in fewer than 100 years in Central Europe.