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Natural sounds

Natural sounds encompass the acoustic phenomena generated by non-human elements within the natural environment, including biological sources such as vocalizations and geophysical processes like , flowing water, and rainfall. These sounds form a core component of scapes, which represent the perceived acoustic environment influenced by context and human interpretation, as defined by the (ISO 12913-1:2014). In ecosystems, natural sounds facilitate essential wildlife communication, serve as indicators of biological health, and contribute to the overall dynamics of wilderness areas. Prominent examples of natural sounds include birdsong, which dominates biological acoustics and aids in territory defense and , and water-related noises from streams or waves, which provide a calming geophysical backdrop. Research demonstrates that exposure to these sounds yields significant benefits for humans, such as reduced and annoyance (Hedges' g = −0.60) and enhanced positive affect and (Hedges' g = 1.63), with water sounds showing particularly strong restorative effects (Hedges' g = 2.01). In national parks, where natural sounds are audible at varying levels—biological sounds at approximately 59% and geophysical at 19% in urban-adjacent sites—they foster a and immersion, supporting visitor experiences and conservation efforts under policies like the U.S. National Park Service's of 1916. The study and preservation of natural sounds have gained prominence through initiatives like the National Park Service's Natural Sounds and Night Skies Division, established in 2000, which addresses threats from anthropogenic noise to maintain ecological integrity and human appreciation of these auditory resources. Despite their ubiquity, only about 11% of monitored sites in U.S. national parks exhibit high audibility of natural sounds with minimal human interference, underscoring the need for ongoing protection to counteract and .

Fundamentals

Definition and Scope

Natural sounds refer to auditory phenomena generated by non-human processes in the , encompassing abiotic sources—such as , flow, and geological events (collectively termed geophony)—and biotic sources from living organisms, including animal vocalizations and movements (termed biophony). This definition explicitly excludes anthropogenic sounds, or anthrophony, which arise from human activities like machinery or urban noise, thereby focusing on the intrinsic acoustic elements of unaltered ecosystems. The scope of natural sounds spans a broad of frequencies and intensities, extending beyond the human audible range of approximately 20 Hz to 20 kHz. , below 20 Hz, includes rumbles that often fall in the 14–35 Hz range with components dipping under 20 Hz for long-distance communication, while above 20 kHz encompasses echolocation pulses typically sweeping from 20 to 110 kHz. variations are equally diverse, ranging from faint incidental noises like rustles at around 20–40 to powerful events such as thunder reaching 120 dB or more, all modulated by propagation through natural media like air, water, or soil. Natural sounds are fundamentally classified into abiotic and categories, with further distinctions within biotic sources between intentional productions—such as deliberate animal calls for or territory —and incidental ones, like unintentional scraping or movement sounds from organisms. Abiotic sounds, by contrast, are generally incidental outcomes of physical processes, exemplified by rustling leaves. This framework delineates inclusions like thunder (abiotic) and bird songs ( intentional) while excluding human-generated noises such as hums or musical instruments, ensuring a clear boundary for studying ecological acoustics.

Historical Context

Human understanding of natural sounds traces back to ancient indigenous knowledge systems, which integrated observations of animal vocalizations for tracking, navigation, and cultural transmission. For instance, Aboriginal Australian traditions incorporate animal sounds into storytelling and environmental awareness, reflecting deep ecological insights passed down through generations. Similarly, early Western philosophers documented these phenomena; in his History of Animals (circa 350 BCE), Aristotle described bird songs, noting that young songbirds learn and refine their vocalizations by imitating adults around them. The marked a pivotal shift with the advent of sound recording technology, enabling the preservation of natural auditory phenomena. In 1857, French inventor Édouard-Léon Scott de Préfontaine developed the , a device that transcribed airborne waves—potentially including natural sources like voices or environmental noises—onto soot-covered paper as visual waveforms for scientific study. This innovation facilitated early attempts at capturing wildlife sounds, culminating in the first known phonographic recording of a bird call in 1889, a captive Indian shama's song at the Frankfurt Zoo, which demonstrated the feasibility of documenting avian vocalizations. The 20th century formalized the scientific study of natural sounds through the emergence of bioacoustics, spurred by post-World War II technological adaptations. The sound spectrograph, originally devised during the war for voice identification, became widely available in the late 1940s and allowed researchers to visualize frequency and time patterns in animal calls, revolutionizing analysis of complex vocal behaviors. In the 1970s, ornithologist Luis Baptista advanced avian bioacoustics by investigating song learning and dialects in species like white-crowned sparrows, establishing key principles of vocal culture in birds. The field's institutionalization was furthered by the founding of the in 1969, which fostered global collaboration on animal sound research. Entering the 21st century, computational tools have transformed bioacoustics, with enabling automated analysis for assessment. Projects in the 2020s employ algorithms to process vast audio datasets from passive recorders, identifying presence and ecological health in real time, such as through models trained on bird and calls. Concurrently, studies since 2010 have linked to alterations in natural sound patterns, documenting shifts in animal vocal timings and frequencies due to warming temperatures and habitat disruption, offering acoustic indicators of broader environmental decline.

Abiotic Natural Sounds

Atmospheric Sounds

Atmospheric sounds encompass acoustic phenomena arising from weather-related processes and air movements in the atmosphere, distinct from seismic or sources. These sounds are primarily generated through rapid changes, , and particle interactions with air or surfaces, propagating as at speeds influenced by environmental conditions. In air at (20°C), travels at approximately 343 meters per second, though this varies with and , affecting how distant events like storms are perceived. Thunder represents one of the most intense atmospheric sounds, produced when heats surrounding air to temperatures up to 30,000°C, causing rapid expansion that generates a akin to a . This explosive expansion creates the initial crack or peal, while the characteristic rumble results from the irregular path of the lightning channel and echoes from multiple return strokes within a single flash, as well as by atmospheric layers. The sound's can reach 120 decibels near the source, diminishing with distance due to geometric spreading and . Wind-generated sounds arise from aerodynamic as air flows over irregular surfaces, such as terrain, vegetation, or structures, producing whooshes, whistles, or howls through and pressure fluctuations. The frequency content shifts with : gentle breezes yield higher-pitched whooshes from small-scale eddies, while high winds in storms like hurricanes generate dominant low-frequency components (below 100 Hz) due to large-scale and resonant interactions. levels correlate with , following a power-law relationship where intensity increases nonlinearly above 10 m/s, often exceeding 80 dB in gale-force conditions. Precipitation sounds, such as those from , , or , stem from the impacts of falling particles on surfaces like ground, , or foliage, exciting vibrations that radiate as acoustic energy. produces a from larger droplets (over 2 mm ) creating discrete low-frequency impacts, transitioning to a continuous hiss from finer due to high-frequency collisions at rates exceeding thousands per second. Sound intensity scales with rainfall rate and drop size distribution, with heavier (over 25 mm/h) generating up to 70 , modulated by surface material—hard surfaces amplify high frequencies, while soft ones dampen them. Tornadoes produce a distinctive roaring akin to a natural , originating from intense low-pressure dynamics and the of , which generates chaotic through collisions and aerodynamic . Pressure drops within (as low as 100 hPa below ambient) drive radial inflows at speeds over 100 m/s, contributing to the low-frequency roar (20-200 Hz), while flying adds impulsive higher-frequency components. Close-range sound levels can exceed 100 , making it one of the loudest atmospheric phenomena, though below 20 Hz often precedes the audible roar, detectable kilometers away. Auroral sounds, though rarer and subtler, manifest as crackling or hissing during intense geomagnetic activity, linked to charged particles from precipitating into the upper atmosphere and inducing electromagnetic resonances. Confirmed by field recordings in , these discrete pops and crackles occur at altitudes of 70-100 meters, synchronized with auroral movements and potentially amplified by atmospheric inversions or —global electromagnetic cavity modes excited by but modulated here by particle fluxes. The sounds are faint, typically under 40 dB, and audible only in quiet, cold conditions near the poles.

Geological and Hydrological Sounds

Geological and hydrological sounds encompass acoustic phenomena generated by physical processes within the Earth's solid crust, liquid bodies, and formations. These sounds arise from mechanical disruptions, , and pressure changes, often manifesting as low-frequency rumbles, booms, or continuous that can propagate over long distances. Unlike atmospheric sounds, which involve gaseous media, these are primarily transmitted through solids, liquids, or , providing insights into subsurface and surface dynamics. Earthquake sounds typically originate from the sudden release of energy along fault lines, producing low-frequency rumbles associated with the propagation of seismic waves. Primary (P) waves, which are compressional, travel at speeds of approximately 5-8 km/s in the Earth's crust, arriving first and generating initial infrasonic signals below 20 Hz that humans may perceive as distant thunder. Shear (S) waves follow at 3-4 km/s, contributing to more intense ground shaking and associated audible low-frequency noises, such as booms or rumbles reported during events. Foreshocks and aftershocks extend these acoustic signatures, with infrasound detection enabling early warning systems by identifying P-wave arrivals seconds to minutes before damaging S-waves reach populated areas. Volcanic eruptions generate explosive booms from rapid gas release during magma ascent and eruption, creating high-pressure acoustic pulses that can reach sound pressure levels up to 180 dB near the source, as exemplified by the 1883 Krakatoa event where pressures equivalent to 172 dB were recorded 160 km away. These infrasonic signals, often in the 0.01-20 Hz range, propagate globally and aid in monitoring eruption dynamics. Lava flows produce hissing sounds from interactions with air or water, resulting from degassing and thermal cracking, which contribute to a broader spectrum of continuous low-frequency noise during effusive activity. Ice cracks, particularly from glacial calving, produce booming sounds due to the sudden release of accumulated as large masses detach and fall into water, generating seismic and acoustic waves from the mechanical stress of fracturing. These events, studied in the context of , reveal increasing calving rates linked to warming temperatures, with sounds serving as indicators of stability and mass loss in polar regions. Hydrological sounds stem from water movement, characterized by turbulence and impact. River rapids create white noise through chaotic fluid flow over obstacles, producing a broad-spectrum roar from turbulent eddies that spans audible frequencies. Waterfalls generate a powerful roar via air entrainment, where falling water traps and compresses air bubbles, resulting in low-frequency vibrations and infrasound around 2-3 Hz that dominate the acoustic profile. Ocean waves crashing exhibit frequency spectra peaking at 0.1-1 Hz, driven by wave breaking and air-water interactions, which produce rhythmic booms and contribute to ambient ocean noise levels. Tsunami infrasound propagation, as observed following the 2004 Indian Ocean event generated by the Sumatra-Andaman , involves low-frequency atmospheric waves excited by the sea surface displacement, detectable thousands of kilometers away via global monitoring networks. These signals, captured at infrasound stations like , highlight the coupling between ocean dynamics and atmospheric acoustics for disaster detection.

Biotic Natural Sounds

Animal Vocalizations

Animal vocalizations encompass a diverse array of sounds produced by s primarily for communication, including territory , mate attraction, social bonding, and predator deterrence. These sounds are generated through specialized anatomical structures and exhibit adaptations suited to various environments, from terrestrial habitats to realms. In mammals, vocalizations often involve low-frequency calls that travel long distances, while utilize complex for reproductive purposes. Amphibians and reptiles produce simpler calls, frequently tied to or , highlighting the evolutionary divergence in vertebrate sound production mechanisms. Among mammals, howls serve as a key territorial signal in species like wolves (Canis lupus), where packs use them to maintain spacing and advertise presence over several kilometers, reinforcing social cohesion and deterring rivals. Elephants (Loxodonta africana and Elephas maximus) employ rumbles in the 1-20 Hz range for long-distance communication, detectable over distances exceeding 10 km under favorable atmospheric conditions, allowing coordination of group movements and family reunions. In contrast, lions (Panthera leo) produce powerful roars reaching up to 114 dB at 1 meter, functioning to claim territory and intimidate competitors, with these low-frequency bursts (around 36-81 Hz) propagating effectively across landscapes. mammals, such as humpback whales (Megaptera novaeangliae), generate intricate songs with fundamental frequencies starting as low as 20 Hz and extending to 24 kHz, featuring repetitive patterns of themes and phrases that evolve culturally within populations, primarily by males during breeding seasons; these songs can propagate thousands of kilometers but are increasingly disrupted by noise, which masks low-frequency components and alters singing behavior. Bird vocalizations demonstrate remarkable complexity, particularly in songbirds, where males produce elaborate songs to attract mates and defend territories. For instance, the (Luscinia megarhynchos) delivers songs comprising up to 200 distinct phrases, showcasing syntactic structure and improvisation that signal cognitive and physical fitness to potential partners. Alarm calls in birds, such as those from fairy-wrens (Malurus spp.), are typically short, high-pitched, and narrow-bandwidth signals peaking around 7-9 kHz, enabling rapid warning of aerial predators while minimizing location cues to the threat. These calls contrast with songs by prioritizing speed and urgency over duration. In amphibians, frogs (Anura) produce croaks primarily for mating advertisement, using vocal sacs to amplify sounds generated by laryngeal vibration; these sacs inflate with air from the lungs, resonating calls in a typical range of 500-5000 Hz to attract females over short distances in environments. Reptiles like snakes (Serpentes) lack true but generate defensive hisses through forceful expulsion of air from the lungs via the , creating a rasping noise that mimics more dangerous threats and deters predators without requiring specialized organs. The primary mechanisms of sound production in vertebrates involve vibration of anatomical structures driven by airflow. In mammals, including cetaceans, sounds arise from laryngeal vibration, where exhaled air passes over vocal folds to produce fundamental frequencies modulated by the vocal tract. Birds, however, possess a unique syrinx at the tracheobronchial junction, allowing independent control of two sound sources for dual-voice singing and precise independent of the larynx. Evolutionary adaptations, such as in vocal organs, further enhance these capabilities; for example, male songbirds often have larger syringes and associated muscles than females, correlating with more complex singing behaviors and enabling dimorphic repertoires for mate attraction.

Invertebrate and Plant Sounds

and produce a variety of sounds through mechanical means, distinct from the vocalizations of vertebrates, often serving roles in communication, , and reproduction. Among , crickets generate sounds via , where specialized structures on their wings are rubbed together to produce frequencies typically ranging from 3 to 4 kHz. This mechanism allows males to attract mates and establish territory, with the resulting chirps propagating through air and substrates. Bees, such as honeybees, create buzzing sounds primarily from rapid wingbeats at approximately 230 Hz during flight and activities. These vibrations not only facilitate but also play a key role in , where the oscillations dislodge from flowers, enhancing reproductive success for both the and the . Moths produce ultrasonic sounds in the range of 20 to 100 kHz for and , often using specialized abdominal or wing structures to emit low-intensity clicks that deter predators or signal to potential mates. Beyond insects, other employ percussion and vibration for acoustic signaling. Spiders generate substrate-borne vibrations through or , producing low-frequency signals between 1 and 300 Hz that travel through threads or surfaces to communicate during or prey detection. use head-banging, where soldiers rapidly strike their heads against walls or the ground at rates up to 11 times per second, creating vibrational knocks that propagate as alarm signals to alert the colony to threats. In marine environments, snapping shrimp ( family) produce some of the loudest biological sounds through : a specialized snaps shut, releasing a that collapses to generate brief pulses reaching up to 190 dB re 1 μPa at 1 m, primarily for territorial defense and communication on coral reefs. Plants contribute to natural soundscapes via passive and active mechanical processes, often triggered by environmental stresses or physical interactions. Wind-induced rustling arises from between leaves and branches, generating audible sounds as air flows cause petioles and foliage to oscillate and shed vortices. Certain , like acacias, exhibit explosive seed pod dehiscence, where drying pods split and curl to propel seeds with audible popping sounds, aiding dispersal in arid habitats. Recent research has revealed that stressed , such as tomatoes and , emit ultrasonic clicks in the 20–100 kHz range, with water-deprived individuals producing 30–50 such bursts per hour, potentially signaling distress to nearby animals or conspecifics. These sounds in and are predominantly non-laryngeal, relying on (e.g., in and spiders), percussion (e.g., termite head-banging and seed pod explosions), or aerodynamic vibration (e.g., wingbeats and leaf rustles). Ecologically, such mechanical acoustics fill specific niches, including signaling where buzzes vibrate flowers to release , thereby promoting cross-species interactions essential for . In coral reefs, snapping pulses contribute to the ambient , potentially aiding larval settlement and ecosystem monitoring.

Ecological Role

In Ecosystems and Communication

Natural sounds play a crucial role in facilitating communication among , particularly in territorial defense and . In , serves as an acoustic signal to deter intruders and maintain exclusive territories, with experimental playback studies demonstrating that simulated high-performance significantly reduce the likelihood of territorial intrusion by eliciting stronger avoidance responses from conspecific males. For instance, in territorial interactions, can minimize overlap in defended areas by signaling occupancy and aggressive intent, thereby reducing direct confrontations and energy expenditure. Similarly, in amphibians, choruses synchronize calling patterns to enhance success; male túngara frogs (Engystomops pustulosus) adjust their call timing to achieve near-synchronous emission within 100 ms of neighbors, which amplifies collective signal detectability for females while minimizing interference. Soundscapes in act as indicators of and health, reflecting underlying trophic dynamics. The dawn chorus, a collective burst of avian vocalizations at sunrise, provides a measurable index of and integrity; metrics like the Bird Dawn Chorus Strength (BDCS), derived from acoustic recordings, correlate positively with bird diversity and vegetation quality in natural , allowing non-invasive monitoring of environmental conditions. In trophic interactions, predator vocalizations trigger anti-predator responses in prey, suppressing their acoustic activity and altering community sound profiles; for example, (Odocoileus hemionus) exhibit heightened vigilance and reduced vocalizations upon hearing predator calls, which can propagate through food webs to influence lower trophic levels in acoustic trophic cascades. Organisms partition acoustic niches to minimize interference in shared environments, optimizing signal transmission. Marine mammals exemplify this through frequency segregation: baleen whales produce low-frequency calls (typically 10–200 Hz) for long-distance communication across ocean basins, while odontocetes like dolphins emit high-frequency echolocation clicks (up to 130 kHz) for short-range and , reducing masking and enabling coexistence in dense populations. This partitioning enhances in noisy soundscapes, where overlapping frequencies could degrade signal clarity. Symbiotic interactions also leverage natural sounds, particularly in mutualisms. Bat-pollinated have evolved acoustic adaptations, such as reflective floral structures that enhance echolocation signals; for example, certain columnar cacti like Espostoa frutescens feature ultrasound-absorbing zones around inflorescences that create distinct echo contrasts, guiding nectar-feeding bats (e.g., Anoura fistulata) precisely to flowers and increasing rates. These passive acoustic cues complement olfactory and visual signals, fostering efficient -insect and -mammal symbioses. Recent 2020s research highlights emerging roles of in , including sound-mediated processes that influence . Studies have shown that specific sound vibrations stimulate production in , enhancing seed viability and potentially aiding dispersal mechanisms by altering fruit dehiscence or attracting dispersers; for instance, sound vibrations at 250 Hz applied to increase levels by up to 200%, which may indirectly support dispersal through improved seed quality and animal attraction. This underscores sound's integrative function in processes beyond .

Human Impacts and Conservation

Human activities profoundly disrupt natural soundscapes through , which masks essential biotic signals and impairs ecological communication. In environments, and noise overlap with the frequency bands of bird vocalizations, requiring birds to achieve a of approximately 26 dB for detection—which is 6 dB higher than for humans—and effectively halving the communication distance for species like great tits. Similarly, in marine ecosystems, shipping generates low-frequency that interferes with whale and , causing behavioral changes such as avoidance of noisy areas, altered dive and foraging patterns, and increased collision risks due to impaired detection of vessels, as observed in humpback whales. These disruptions extend to aquatic environments, where ocean vessel elevates ambient levels, masking cetacean calls and complicating long-distance coordination during seasonal migrations. Climate change further alters natural sounds by shifting phenological timings and diminishing hydrological acoustics. Warmer temperatures have advanced frog breeding choruses, with ornate chorus frogs in initiating calls 37.2 days earlier since 1979, potentially desynchronizing them from prey availability or mates. exacerbates this by reducing water flows, leading to quieter stream and river soundscapes; for instance, in California's Sugarloaf Ridge State Park, diminished cascades and ripples have contributed to a fivefold drop in overall biophony since 2004. Indirectly, influences acoustic behaviors by advancing the seasonal onset of dawn and singing in European songbirds like and blackbirds, disrupting natural circadian rhythms and potentially affecting through altered territorial signaling. Conservation efforts aim to mitigate these impacts by establishing protected acoustic environments and implementing regulatory measures. The U.S. Service's 2006 Management Policies (Section 4.9) mandate the preservation of natural soundscapes, including the creation of quiet zones through monitoring and restrictions on motorized activities to restore degraded areas. In marine contexts, the International Maritime Organization's 2014 Guidelines for the Reduction of Underwater from Commercial Shipping, revised in 2023, provide voluntary standards for vessel design and operation to minimize radiated , with an ongoing experience-building phase through 2026 to inform potential mandatory regulations. Monitoring tools play a crucial role in assessing and safeguarding via acoustic data. Passive acoustic sensors enable non-invasive, long-term recording of soundscapes, allowing researchers to quantify and detect intrusions through indices like acoustic complexity. Global initiatives, such as the Biodiversity Monitoring Institute's Bioacoustic Unit and its 2025 HawkEars project, deploy autonomous recording units to analyze bird and calls, supporting by tracking climate-induced shifts and noise effects across Canadian ecosystems.

Human and Cultural Dimensions

Perception and Physiological Effects

Human hearing typically encompasses frequencies from 20 Hz to 20 kHz, with the greatest occurring between 2 and 5 kHz, a range that aligns closely with many natural sounds such as bird calls, which often fall between 1 and 8 kHz. This sensitivity peak enhances detection of environmental cues essential for survival, like predator warnings or foraging signals in ancestral habitats. Natural sounds elicit varied physiological responses, including relaxation from rain sounds, which are commonly featured in autonomous sensory meridian response () content to promote calmness. Conversely, infrasound from storms, below 20 Hz, may induce unease or vertigo by stimulating the , triggering symptoms akin to . These reactions underscore the body's innate tuning to acoustic environments, where low frequencies signal potential threats. In therapeutic contexts, exposure to nature soundscapes has demonstrated stress-reducing effects, with studies from the showing significant reductions in levels in participants after listening sessions. A 2025 scoping further confirmed the stress-reducing effects of natural s among various sound interventions. Such benefits may from evolutionary adaptations to savanna soundscapes, where early hominins developed enhanced mid-frequency hearing for short-range communication in open terrains, differing from forest-dwelling . Individual differences influence perception, as age-related hearing loss () progressively impairs high-frequency detection, often diminishing awareness of insect chirps or bird songs above 4 kHz. Recent 2024 meta-analyses support the by linking natural sounds to improved outcomes, including reduced anxiety and enhanced emotional recovery.

Cultural Representations

Natural sounds have long been represented in literature through onomatopoeic devices that mimic auditory phenomena, such as the "boom" or "crash" used to depict thunder in and mythological narratives across cultures. These words evoke the explosive resonance of storms, often tied to divine or supernatural entities, as in tales where thunder symbolizes the wrath of gods like Thor. In visual , Romantic-era painters like captured the implied auditory drama of natural tempests in seascapes, such as Seascape with Storm Coming On (c. 1840), where turbulent waves and skies suggest the roar of wind and crashing surf, blending visual tumult with sonic inference. In music and media, natural sounds are integrated via field recordings to create immersive atmospheres, notably in Brian Eno's ambient works like Ambient 4: On Land (1982), which incorporates environmental noises such as wind and water to evoke landscapes and blur the line between composition and nature. Film sound design similarly employs these elements for narrative depth; in Star Trek IV: The Voyage Home (1986), humpback whale songs—drawn from Roger Payne's 1970 recordings on the LP Songs of the Humpback Whale—form a central motif, symbolizing interstellar communication and highlighting cetacean vocalizations as a bridge between species and eras. Indigenous practices frequently feature imitations of natural sounds in rituals and oral traditions, as seen in Native American flute music where instruments like the courting flute, often adorned with bird motifs, replicate calls to invoke spiritual connections during ceremonies for , , and invocation. Storytelling among these communities employs animal sound metaphors to convey moral and ecological lessons, portraying creatures as "the people" whose vocalizations—such as howls or chirps—embody relational and with the in narratives passed orally across generations. In modern , natural sounds drive experiential content like videos featuring rain, which have amassed billions of views collectively since , tapping into their soothing qualities for relaxation and sensory triggers popular on platforms like and . Virtual reality applications further enhance immersion through spatialized natural soundscapes, where ambient elements like birdsong and rustling leaves significantly boost perceived presence and realism, as demonstrated in studies showing improved user involvement in simulated environments (e.g., effect sizes η² = 0.341–0.583). Global research underscores the integration of natural sounds in non-Western traditions, examining how wind instruments in South American cultures, such as flutes and whistles, replicate environmental acoustics to mediate and boundaries during ceremonies. These studies highlight sound healing practices worldwide, where sonic imitations of —via drums, chants, and aerophones—facilitate physical and emotional restoration in communal rituals.

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