1. Introduction
This paper uses a literature review research methodology to provide a comprehensive analysis and summary of the impacts of volcanic ash on both environment and human beings. This study provides a comprehensive analysis of the composition of volcanic ash and its effects on several aspects such as climate, ecosystems, soils, plants, water quality, wildlife, and human health. It also explores the strategies and measures taken to mitigate the hazards associated with volcanic ash. The significance of this study lies in the comprehensive analysis of volcanic ash as a natural occurrence and a comprehensive understanding of its impacts on the environment and human beings, which will help us to better understand the dangers of volcanic ash poses to ecosystems and human societies, and enable us to suggest appropriate measures to address these threats [1]. This paper presents a comprehensive investigation and examination of volcanic ash, serving as a theoretical foundation and point of reference for research in related areas. Additionally, it provides suggestions for disaster management and ecological protection. However, additional comprehensive research is required to investigate the composition, characteristics, and methods by which volcanic ash affects the environment and human beings. Furthermore, there is a need to develop more efficient early warning systems and preventive measures.
2. Volcanic ash
2.1. Definition and composition of volcanic ash
Volcanic ash particles typically exhibit an angular and uneven morphology. Volcanic ash is generated through the explosive disintegration of magma and rock, resulting in the formation of particles with diverse forms and sizes. Volcanic ash has a relatively low density compared to other types of sediments and rocks, because it mainly consists of small, light glass particles and mineral crystals. The color of volcanic ash can vary between white, grey, brown, or black, and it may consist of many minerals and compounds that contribute to its unique coloration. The chemical composition of volcanic ash can vary greatly depending on the specific volcano and the composition of the emitted magma . It usually contains a mixture of silicate minerals such as quartz, feldspar and mica, together with volcanic glass and other mineral crystals. Volcanic ash contains several elements including silicon, aluminium, iron, calcium, sodium and potassium [2], these elements typically reflect geochemical signatures derived from magma.
2.2. Distribution of volcanic ash
Volcanic ash has the potential to disperse both locally and worldwide, contingent upon the magnitude and strength of the eruption, as well as prevailing weather conditions and wind patterns. Volcanic ash can cover surrounding areas, buildings, roads and crops. These factors can have significant impacts on agriculture, transportation and infrastructure. In some cases, thick ash can cause the collapse of buildings and the disruption of aviation transport. Volcanic ash can also be carried over long distances by the wind. Minuscule particles of volcanic ash have the ability to traverse vast distances of thousands of kilometers within the atmosphere, enveloping large areas and even encircling the entire planet. This can have a significant impact on air quality, climate and patterns of weather [3]. The dispersion of volcanic ash is determined by an intricate interaction of various factors, such as the magnitude and strength of the eruption, atmospheric wind patterns, and weather conditions.
3. Hazards of volcanic ash
3.1. Impact on air quality
Volcanic eruptions produce ash while releasing large amounts of gases. Carbon dioxide (CO2), silica (SO2), methane (CH4), carbon monoxide (CO), nitrogen oxides (NOx), and water vapor are considered to be the most significant among these substances. Carbon dioxide and methane are among the greenhouse gases that cause the earth's temperature to rise, contributing to the phenomenon of global warming. Carbon monoxide is toxic and flammable and can negatively affect human, animal and plant health.Ozone is formed when nitrogen oxides undergo a reaction with oxygen present in the environment. Ozone, an air contaminant, poses significant risks to both human health and ecological systems. When large amounts of water vapour cool from the crater, volcanic precipitation is formed, which may have a direct impact on ecosystems and water resources in nearby areas [4]. Volcanoes also release large amounts of ash and particulate matter. These fine particles can float hundreds of kilometres in the atmosphere and last for several months. These particles can have a long-term impact on environmental ecosystems. This is because the particulate matter combines with atmospheric water vapor to create acidic fallout, which can pollute soil, vegetation, and water sources.
3.2. Impact on global climate
The introduction of volcanic ash into the stratosphere by volcanic eruptions exerts a direct influence on the global climate. In particular, sulphur-containing gases, primarily SO2, and increased levels of sulphuric acid aerosol content are major contributors to climate change. SO2 released by volcanic eruptions is oxidised in the stratosphere into small sulphuric acid aerosol particles, which range in size from 0.1 to 1 μm. Aerosols are dispersed globally through stratospheric circulation. Due to the stability of stratospheric circulation, aerosols can endure in the stratosphere for extended durations, typically lasting one year or longer. This allows them to efficiently reflect and absorb solar radiation, resulting in a decrease in surface temperatures. Consequently, the earth's surface and lower atmosphere cool down, partially decelerating the pace of global warming observed in the twentieth century [5]. Super-volcanic activity can have enduring effects, such as triggering a positive albedo and radiation feedback mechanism in snow and ice by affecting snow and ice extent at high latitudes, or influencing changes in photosynthesis by affecting the state of the vegetation, which can have a more significant impact on Earth's climate change.
3.3. Impact on water quality
The impact of volcanic ash on water quality depends on the quantity and composition of the ash, the type of water body and environmental conditions. Volcanic ash deposition in rivers and streams can lead to sedimentation, reducing water clarity and affecting aquatic ecosystems. Sediments possess significant quantities of essential nutrients, including nitrogen and phosphorus, which have the potential to facilitate the proliferation of algae and other aquatic flora, thereby contributing to eutrophication and the deterioration of water quality. Additionally, sediments can induce pH changes in water bodies, resulting in increased acidity and posing risks to aquatic organisms. Simultaneously, volcanic ash may contain hazardous substances, such as heavy metals and toxic gases, which have the capacity to pollute both surface water and groundwater, directly affecting the quality of human drinking water sources. When large amounts of volcanic ash are deposited, they may clog waterways and cause flooding, affecting water flows and having a significant impact on water quality and aquatic ecosystems.
3.4. Impact on soil and plants
Volcanic ash can have both positive and negative effects on plants, depending on the amount and composition of the ash, as well as the type of plant and stage of growth. When the composition of volcanic ash is suitable, it has the potential to enhance plant development and enhance soil fertility through the introduction of nutrients such as nitrogen, phosphate, and potassium. Additionally, the presence of ash deposits can lead to soil compaction, resulting in a reduction of pore space and therefore impacting the soil's capacity to retain water and nutrients. Nevertheless, the accumulation of substantial amounts of volcanic ash on the soil surface can result in the deterioration of the soil structure, impeding the infiltration of water and the establishment of roots, thereby impacting plant growth. Volcanic ash accumulation can also increase the risk of erosion, especially in areas with high rainfall or sloping topography [6].
Sometimes volcanic ash can also contain toxic compounds such as sulphur dioxide, hydrogen sulphide and fluorine, which are harmful to plant growth and health, as well as increasing soil acidity, altering the ability of plants to access nutrients and reducing soil fertility. The accumulation of ash on plants can have detrimental effects on their growth and development, resulting in direct physical harm that hampers photosynthesis, transpiration, and overall growth. The pollination process between plants can be disrupted by volcanic ash, resulting in detrimental effects on reproductive structures and a subsequent decrease in food output.
3.5. Impacts on wildlife
Volcanic ash can cause respiratory problems, ocular irritation, and dermal irritation in animals. Additionally, it has the potential to cause harm to the feathers, fur, and scales of animals, so impeding their ability to effectively regulate body temperature and safeguard themselves against adverse weather conditions. Volcanic ash can also damage food sources and obstruct the visibility of plants and vegetation, making it difficult for herbivores to find food. Additionally, it has the potential to pollute water supplies, so impeding animals' access to uncontaminated drinking water. In severe cases, animal habitats can be destroyed. Volcanic eruptions can destroy the habitats of many species, especially those that live in areas near volcanoes [7]. Volcanic ash can bury burrows and nests, as well as cause landslides and other geological hazards. Animals may change their behaviour in response to a volcanic eruption. For example, birds may stop singing and mammals may become more nocturnal to avoid exposure to ash and other hazards.
3.6. Impact on human health
Humans may experience a number of physical problems if exposed to volcanic ash for long periods of time. The predominant issue is respiratory complications; the act of inhaling volcanic ash can lead to respiratory disorders such as coughing, wheezing, and difficulty breathing. This is due to the ash's composition, which comprises minute particles capable of penetrating deeply into the lungs, resulting in irritation and inflammation [8]. In addition, the dust is abrasive and can irritate the delicate tissues of the eyes, causing eye irritation, redness and tearing. Moreover, because the ash contains harmful chemicals and heavy metals that can be toxic when ingested ingested, volcanic ash can cause gastrointestinal problems, including nausea, vomiting and diarrhoea.
4. Volcanic ash mitigation and hazard response methods
4.1. Early warning systems for volcanic eruptions
Volcanic ash can cause various detrimental effects on both persons and the environment. Therefore, it is crucial for individuals to implement suitable preventive and remediation measures following an eruption in order to mitigate potential risks. Volcanic eruptions exhibit a range of conditions, spanning from consistent magma flows to the manifestation of intense eruptions. Ensuring the timely, dependable, and uniform dissemination of information regarding volcanic ash is crucial in order to minimize the safety hazards faced by aircraft that come into contact with volcanic ash. In order to respond effectively and in a timely manner to the weather effects of volcanic ash, a robust detection and warning system is required. The detection system should be able to detect volcanic activity and ash as it occurs. Weather forecasting and dust dispersion modelling should also be established, alongside the prompt dissemination of detection data to both governmental bodies and the general public [9].
4.2. Methods for predicting the distribution of volcanic ash
There are four main key methods for predicting volcanic ash distribution. Numerical modelling predicts ash dispersion through computer simulations based on factors such as eruption source, eruption intensity, atmospheric conditions and wind patterns, and uses complex algorithms and equations to model the behaviour of ash particles. Remote sensing, on the other hand, monitors volcanic ash clouds from the air through satellites and other high-tech instruments to estimate their location, extent and movement, providing data to support the prediction of the potential impact of an eruption [10]. Volcanic ash dispersion models, which are specialised computer models that simulate the movement of volcanic ash in the atmosphere, taking into account factors such as particle size, wind speed and other factors, are critical in areas such as aviation safety. Empirical models, on the other hand, use historical data and observations to assess the likely distribution of volcanic ash based on past experience of volcanic activity, which is less refined than the other methods but provides important baseline information. The combined application of these methods can effectively improve the accuracy of volcanic ash predictions, which is essential for reducing the impacts caused by volcanic ash [11].
4.3. Ecological restoration measures
In addition to reducing the harm caused by volcanic ash, we must also learn to use it. Volcanic ash is rich in many nutrients, such as silicon, aluminium, calcium and magnesium. Volcanic ash can be utilized to enhance soil fertility and enhance the physical composition of the soil. In addition, volcanic ash creates a layer of mulch that can protect plants from climate extremes and ultraviolet rays. It also has an insulating and moisturising effect, mitigating the effects of drought and cold on plants. Volcanic ash is a natural environmental sustaining substance that has the ability to rapidly restore the ecological equilibrium following an eruption. It can provide biological habitat and sources of nutrients that promote the growth and reproduction of plants and animals. Volcanic ash filters impurities from water sources and purifies water. It exhibits the ability to adsorb deleterious elements and diminish the concentration of heavy metals and organic compounds within water, hence safeguarding the well-being and integrity of water supplies.
5. Case study
The Eyjafjallajökull glacier volcano in Iceland, known for its recurrent eruptions since the Ice Age, experienced a rapid outburst on October 2, 1996, following a period of over a millennium of stillness. Following the eruption, large quantities of lava and ash were ejected into the air and subsequently fell to the cold ground. Upon exposure to the air, these substances rapidly cooled and consolidated, resulting in the formation of a substantial coating of volcanic ash. The ash obstructed the sunshine, resulting in a significant decrease in temperatures in Iceland, leading to the coldest winter ever recorded. The ash resulting from this volcanic eruption settled on the riverbed, impeding the water flow and creating rapid river flooding. This resulted in the destruction of agricultural land, the erosion of residential structures, the loss of livestock, and the disruption of people's life.The eruption led to the widespread closure of European airspace, the cancellation of tens of thousands of flights, and significant economic losses for airlines and the tourism industry, estimated to be in the billions of dollars. Simultaneously, numerous reservoirs experienced excessive loading as a consequence of the swift escalation in water levels, resulting in significant water scarcity in certain regions [12]. Subsequently, this occurred multiple times in the years 1821, 1822, 1823, and 2010, in that order. On 26 February 2010, the Icelandic Meteorological Service recorded a series of unusual seismic activity accompanied by crustal spreading. Geophysicists saw this as evidence that magma below the Earth's crust was being pressed into the magma chambers of volcanoes, and that the pressure generated by this process was causing violent crustal dislocations. Seismic activity continues to increase, with nearly 3,000 earthquakes with volcanic sources recorded between 3 and 5 March [13].
Currently, it is imperative that we persist in enhancing our investigation into volcanic phenomena and enhancing our capacity to avert and address the occurrence of volcanic eruption dust weather. This is crucial for safeguarding and upholding the sustainable progress of human civilization. An essential challenge in the study of volcanic soot distribution prediction is ensuring the precision and worldwide scope of the soot distribution. Although current numerical simulation techniques have been able to successfully simulate the spread of volcanic soot, the limitations of data sources and computational accuracy make the simulation results still have some errors. Therefore, it is imperative to enhance the study and refinement of the model, incorporate additional data and employ exact calculation techniques in order to attain greater accuracy and reliability.
6. Conclusion
This paper presents a comprehensive analysis of the impact of volcanic ash on the environment and humans, and proposes appropriate methods of protection and mitigation. However, there are certain limitations in this study. The present study primarily relies on a comprehensive literature review and lacks empirical validation through field investigation and experimentation. Therefore, there may still be some limitations in the understanding of the effects of volcanic ash and coping strategies. Subsequent examinations and experimental studies have the potential to yield a more comprehensive comprehension of the attributes and processes of impact associated with volcanic ash. Furthermore, while this work encompasses a broader array of subjects on the effects of volcanic ash, it lacks a comprehensive and meticulous examination of each individual issue. Further research might investigate the ramifications of volcanic ash on the environment and human populations at a broader and more comprehensive scale. This could involve doing thorough investigations into the underlying mechanisms by which it affects air quality, soil and water quality, as well as biodiversity. Furthermore, the current investigation has not examined the variations in the impacts of volcanic ash on several geographical areas and distinct demographic groups, hence highlighting a potential avenue for future scholarly inquiry.
Future research could further improve the accuracy and real-time nature of volcanic ash prediction and monitoring to better address the threat of volcanic ash to aviation safety, agriculture and human well-being. The field may also delve deeper into the examination of techniques for managing and harnessing volcanic ash, as well as study the innovative applications of volcanic ash, such as its utilization in construction materials, environmental remediation, and agricultural fertilizers [14]. Furthermore, via the integration of diverse study methodologies in the fields of meteorology, geology, and ecology, a more comprehensive understanding of the enduring consequences of volcanic ash on the Earth's system and its correlation with climate change can be attained. Future research has the potential to enhance worldwide collaboration in order to collectively build a comprehensive system for monitoring volcanoes, issuing early warnings, and managing disasters. This collaborative effort aims to enhance the safeguarding of both human and environmental security.
References
[1]. Jones MT. The environmental and climatic impacts of volcanic ash deposition. In: Schmidt A, Fristad K, Elkins-Tanton L, eds. Volcanism and Global Environmental Change. Cambridge University Press; 2015:260-274.
[2]. Bonadonna, C., & Costa, A. (2013). Estimating the volume of tephra deposits: a new simple strategy. Geology, 41(8), 887-890.
[3]. Edwards, M. J., Eychenne, J. & Pioli, L. Formation and dispersal of ash at open conduit basaltic volcanoes: Lessons from Etna.Front. Earth Sci. 9, 709657 (2021)
[4]. Baxter, P. J., & Neri, A. (2017). Impact of volcanic eruptions on agriculture. Agriculture, Ecosystems & Environment, 239, 243-254.
[5]. Dhomse, S. S. et al. Evaluating the simulated radiative forcings, aerosol properties, and stratospheric warmings from the 1963 Mt Agung, 1982 El Chichón, and 1991 Mt Pinatubo volcanic aerosol clouds. Atmos. Chem. Phys. 20, 13627–13654 (2020).
[6]. Schijf, J., Marshak, S., & Berhe, S. M. (2017). Impact of volcanic ash on trees: a review. Journal of Volcanology and Geothermal Research, 343, 36-57.
[7]. Rueden, C.T.; Schindelin, J.; Hiner, M.C.; DeZonia, B.E.; Walter, A.E.; Arena, E.T.; Eliceiri, K.W. ImageJ2: ImageJ for the next Generation of Scientific Image Data. BMC Bioinform. 2017, 18, 529.
[8]. Horwell, C. J. (2018). The health hazards of volcanic ash: a review. Geoenvironmental Disasters, 5(1), 1-15.
[9]. Scott, K. M., Bacon, C. R., & Burgisser, A. (2019). Experimental investigations of tephra transport and sedimentation. Journal of Geophysical Research: Solid Earth, 124(8), 8204-8220.
[10]. Lan Liu. Research on volcanic ash cloud identification method and application for satellite remote sensing data Shanghai: Shanghai University, 2018
[11]. Engwell, S., Mastin, L., Tupper, A. et al. Near-real-time volcanic cloud monitoring: insights into global explosive volcanic eruptive activity through analysis of Volcanic Ash Advisories. Bull Volcanol 83, 9 (2021).
[12]. Möller, R., Möller, M., Kukla, P.A., Schneider, C., 2018. Modulation of glacier ablation by tephra coverage from Eyjafjallajökull and Grímsvötn volcanoes, Iceland: an automated field experiment. Earth Syst. Sci. Data 10, 53–60.
[13]. FU, G., PRATA, F., HAI, X.L., HEEMINK, A., SEGERS, A. and LU, S., 2017. Data assimilation for volcanic ash plumes using a satellite observational operator: a case study on the 2010 Eyjafjallajökull volcanic eruption. Atmospheric Chemistry and Physics, 17(2), pp. 1187-1205.
[14]. A. Costa, A. Folch, G. Macedonio, B. Giaccio, R. Isaia, V. C. Smith(2015). Quantifying volcanic ash dispersal and impact of the Campanian Ignimbrite super-eruption,241(3–4), 634–647.
Cite this article
Zhang,J. (2024). Analysis of the impact of volcanic ash on the environment and human . Theoretical and Natural Science,37,119-124.
Data availability
The datasets used and/or analyzed during the current study will be available from the authors upon reasonable request.
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References
[1]. Jones MT. The environmental and climatic impacts of volcanic ash deposition. In: Schmidt A, Fristad K, Elkins-Tanton L, eds. Volcanism and Global Environmental Change. Cambridge University Press; 2015:260-274.
[2]. Bonadonna, C., & Costa, A. (2013). Estimating the volume of tephra deposits: a new simple strategy. Geology, 41(8), 887-890.
[3]. Edwards, M. J., Eychenne, J. & Pioli, L. Formation and dispersal of ash at open conduit basaltic volcanoes: Lessons from Etna.Front. Earth Sci. 9, 709657 (2021)
[4]. Baxter, P. J., & Neri, A. (2017). Impact of volcanic eruptions on agriculture. Agriculture, Ecosystems & Environment, 239, 243-254.
[5]. Dhomse, S. S. et al. Evaluating the simulated radiative forcings, aerosol properties, and stratospheric warmings from the 1963 Mt Agung, 1982 El Chichón, and 1991 Mt Pinatubo volcanic aerosol clouds. Atmos. Chem. Phys. 20, 13627–13654 (2020).
[6]. Schijf, J., Marshak, S., & Berhe, S. M. (2017). Impact of volcanic ash on trees: a review. Journal of Volcanology and Geothermal Research, 343, 36-57.
[7]. Rueden, C.T.; Schindelin, J.; Hiner, M.C.; DeZonia, B.E.; Walter, A.E.; Arena, E.T.; Eliceiri, K.W. ImageJ2: ImageJ for the next Generation of Scientific Image Data. BMC Bioinform. 2017, 18, 529.
[8]. Horwell, C. J. (2018). The health hazards of volcanic ash: a review. Geoenvironmental Disasters, 5(1), 1-15.
[9]. Scott, K. M., Bacon, C. R., & Burgisser, A. (2019). Experimental investigations of tephra transport and sedimentation. Journal of Geophysical Research: Solid Earth, 124(8), 8204-8220.
[10]. Lan Liu. Research on volcanic ash cloud identification method and application for satellite remote sensing data Shanghai: Shanghai University, 2018
[11]. Engwell, S., Mastin, L., Tupper, A. et al. Near-real-time volcanic cloud monitoring: insights into global explosive volcanic eruptive activity through analysis of Volcanic Ash Advisories. Bull Volcanol 83, 9 (2021).
[12]. Möller, R., Möller, M., Kukla, P.A., Schneider, C., 2018. Modulation of glacier ablation by tephra coverage from Eyjafjallajökull and Grímsvötn volcanoes, Iceland: an automated field experiment. Earth Syst. Sci. Data 10, 53–60.
[13]. FU, G., PRATA, F., HAI, X.L., HEEMINK, A., SEGERS, A. and LU, S., 2017. Data assimilation for volcanic ash plumes using a satellite observational operator: a case study on the 2010 Eyjafjallajökull volcanic eruption. Atmospheric Chemistry and Physics, 17(2), pp. 1187-1205.
[14]. A. Costa, A. Folch, G. Macedonio, B. Giaccio, R. Isaia, V. C. Smith(2015). Quantifying volcanic ash dispersal and impact of the Campanian Ignimbrite super-eruption,241(3–4), 634–647.