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Artykuły w czasopismach na temat „Turbidity”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 25 lipca 2025

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1

Cattaneo, A., N. Babonneau, G. Ratzov, et al. "Searching for the seafloor signature of the 21 May 2003 Boumerdès earthquake offshore central Algeria." Natural Hazards and Earth System Sciences 12, no. 7 (2012): 2159–72. http://dx.doi.org/10.5194/nhess-12-2159-2012.

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Abstract. Shaking by moderate to large earthquakes in the Mediterranean Sea has proved in the past to potentially trigger catastrophic sediment collapse and flow. On 21 May 2003, a magnitude 6.8 earthquake located near Boumerdès (central Algerian coast) triggered large turbidity currents responsible for 29 submarine cable breaks at the foot of the continental slope over ~150 km from west to east. Seafloor bathymetry and backscatter imagery show the potential imprints of the 2003 event and of previous events. Large slope scarps resulting from active deformation may locally enhance sediment inst

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2

Patton, J. R., C. Goldfinger, A. E. Morey, C. Romsos, B. Black, and Y. Djadjadihardja. "Seismoturbidite record as preserved at core sites at the Cascadia and Sumatra–Andaman subduction zones." Natural Hazards and Earth System Sciences 13, no. 4 (2013): 833–67. http://dx.doi.org/10.5194/nhess-13-833-2013.

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Abstract. Turbidite deposition along slope and trench settings is evaluated for the Cascadia and Sumatra–Andaman subduction zones. Source proximity, basin effects, turbidity current flow path, temporal and spatial earthquake rupture, hydrodynamics, and topography all likely play roles in the deposition of the turbidites as evidenced by the vertical structure of the final deposits. Channel systems tend to promote low-frequency components of the content of the current over longer distances, while more proximal slope basins and base-of-slope apron fan settings result in a turbidite structure that

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Kudymov, A. V. "THE MECHANISM FOR CRETACEOUS TURBIDITE DEPOSITION IN LOWER PRIAMURYE." Tikhookeanskaya Geologiya 44, no. 2 (2025): 22–33. https://doi.org/10.30911/0207-4028-2025-44-2-22-33.

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The mechanism for deposition of Cretaceous turbidites in Lower Priamurye, just like all turbidites in general, is based on the hydrodynamic regime in the basin of their accumulation. The scheme of the hydrodynamic regime of turbidite sedimentation is given using the Berriasian-Valanginian basin of the Gorinsky terrane as an example. Sediments from the eastern margin of the Eurasian continent accreted at the continental slope to be moved eastward to its base by turbidity currents created by submarine slumping of sediments. The coarse material of the landslides settled out first, and fine-graine

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Naruse, Hajime, and Kento Nakao. "Inverse modeling of turbidity currents using an artificial neural network approach: verification for field application." Earth Surface Dynamics 9, no. 5 (2021): 1091–109. http://dx.doi.org/10.5194/esurf-9-1091-2021.

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Abstract. Although in situ measurements in modern frequently occurring turbidity currents have been performed, the flow characteristics of turbidity currents that occur only once every 100 years and deposit turbidites over a large area have not yet been elucidated. In this study, we propose a method for estimating the paleo-hydraulic conditions of turbidity currents from ancient turbidites by using machine learning. In this method, we hypothesize that turbidity currents result from suspended sediment clouds that flow down a steep slope in a submarine canyon and into a gently sloping basin plai

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Ono, Kenya, Hajime Naruse, Qifeng Yao, Zhirong Cai, Sojiro Fukuda, and Miwa Yokokawa. "Multiple scours and upward fining caused by hydraulic jumps: implications for the recognition of cyclic steps in the deepwater stratigraphic record." Journal of Sedimentary Research 93, no. 4 (2023): 243–55. http://dx.doi.org/10.2110/jsr.2021.142.

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ABSTRACT Hydraulic jumps control the bypass, erosion, and depositional processes of Froude-supercritical turbidity currents, so they represent a significant process for understanding the development of submarine geomorphology. Hydraulic jumps actively occur from submarine canyons to fans, where the seafloor slope is relatively steep. Turbidites in such areas comprise large-scale bedforms called cyclic steps, and they exhibit complex internal structures, including localized erosion and the accumulation of coarse-grained fining-upward sequences. However, it is unclear which turbidity-current pro

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Van Daele, Maarten, Peter J. Haeussler, Robert C. Witter, Nore Praet, and Marc De Batist. "The Sedimentary Record of the 2018 Anchorage Earthquake in Eklutna Lake, Alaska: Calibrating the Lacustrine Seismograph." Seismological Research Letters 91, no. 1 (2019): 126–41. http://dx.doi.org/10.1785/0220190204.

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Abstract The 30 November 2018 Mw 7.1 Anchorage earthquake caused modified Mercalli intensities of V¼ to V½ at Eklutna Lake (south central Alaska). A few hours after the earthquake, a “dirt streak” was observed on the lake surface, followed by a peak in sediment turbidity values (∼80 times normal) at a drinking water facility, which receives water from the lake through a pipe. These observations hint toward turbidity currents triggered by the earthquake in Eklutna Lake. Here, we study 32 short sediment cores retrieved from across Eklutna Lake and observe a millimeter‐to‐centimeter scale turbidi

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Ho, Viet Luan, Robert M. Dorrell, Gareth M. Keevil, et al. "Dynamics and deposition of sediment-bearing multi-pulsed flows and geological implication." Journal of Sedimentary Research 89, no. 11 (2019): 1127–39. http://dx.doi.org/10.2110/jsr.2019.62.

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ABSTRACT Previous studies on dilute, multi-pulsed, subaqueous saline flows have demonstrated that pulses will inevitably advect forwards to merge with the flow front. On the assumption that pulse merging occurs in natural-scale turbidity currents, it was suggested that multi-pulsed turbidites that display vertical cycles of coarsening and fining would transition laterally to single-pulsed, normally graded turbidites beyond the point of pulse merging. In this study, experiments of dilute, single- and multi-pulsed sediment-bearing flows (turbidity currents) are conducted to test the linkages bet

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8

Pandya, K. L. "Undaturbidite in the Talchir Group, Talchir Gondwana Basin, Orissa." Journal Geological Society of India 33, no. 6 (1989): 556–65. http://dx.doi.org/10.17491/jgsi/1989/330607.

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Abstract A sedimentary sequence constituted of interbedded sheet sandstones and shales and lenticular channel sandstones exhibits a number of sedimentary structures common in turbidites. These are various types of sole marks, graded bedding, ripple-drift cross laminations, parallel laminations and asymmetric current ripples. The sheet sandstones. show characteristic internal vertical arrangement of structures identical to turbidite sequences while the shales are laminated. Besides, a few rolled boulders and cobbles are found within the sequence. The combination of sedimentary structures sugges

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Hidayat, Jafron Wasiq, Karyadi Baskoro, and Rini Sopiany. "Struktur Komunitas Mollusca Bentik Berbasis Kekeruhan Di Perairan Pelabuhan Tanjung Emas Semarang." Bioma : Berkala Ilmiah Biologi 10, no. 2 (2012): 65. http://dx.doi.org/10.14710/bioma.10.2.65-73.

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The breakwater of Tanjung Emas Seaport is designed to absorb seawave as well as increase ships stability.Such water stability will trigger the light and small particles to deposite onto the bottom of the water body,eventhough these are easily re-suspended and initiate to create turbidity. Turbididty is one factor affecting Mollusccommunity. In facing the global climate changes, there will be a seriuos problem triggering the turbidity of theseawater and so do the organims. Researh were aimed to study the benthic Mollusc community in different turbiditylevels. Justified ramdom sampling was appli

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AKA, Natchia, Abou Traoré, Nadi Paul Dangui, and Yao Dakro Albert Gboko. "Suivi de la turbidité et des matières en suspension dans les rivières côtières en milieu tropical : cas de la Mé et de l’Agneby (sud-est de la Cote d’Ivoire)." Journal of Applied Biosciences 183 (March 31, 2023): 19103–22. http://dx.doi.org/10.35759/jabs.183.1.

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Au Sud de la Côte d’Ivoire, l’État fait recours aux rivières côtières Mé et Agnéby pour pallier le déficit en eau potable destinée aux populations. Cependant, la forte turbidité et les concentrations élevées des matières en suspension dans ces cours d’eaux sont des indicateurs de la dégradation de leur qualité. Objectif Cette étude vise à évaluer la dynamique de la turbidité et des Matières en Suspension (MES) au cours du temps. Méthodologie et Résultats Pour ce faire, des mesures journalières de turbidité et de MES ont été réalisées sur un total de 277 échantillons d’eau prélevés dans la Mé e

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11

Normandeau, Alexandre, and D. Calvin Campbell. "Recurrence of turbidity currents on glaciated continental margins: A conceptual model from eastern Canada." Journal of Sedimentary Research 90, no. 10 (2020): 1305–21. http://dx.doi.org/10.2110/jsr.2020.66.

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ABSTRACT Turbidity currents in submarine canyons transport large volumes of sediment and carbon to the deep sea and are known to present a major risk to submarine infrastructure. Understanding the origin, the triggers, the recurrence, and the timing of these events is important for predicting future events and mitigating their impact. Depending on the morphological and latitudinal setting of submarine canyons, different external controls will govern the recurrence of turbidity currents. Here, we assess the recurrence of turbidity currents in shelf-incising submarine canyons off eastern Canada

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12

Hill, Jenna C., Janet T. Watt, Daniel S. Brothers, and Jared W. Kluesner. "Submarine canyons, slope failures and mass transport processes in southern Cascadia." Geological Society, London, Special Publications 500, no. 1 (2020): 453–75. http://dx.doi.org/10.1144/sp500-2019-169.

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AbstractMarine turbidite records have been used to infer palaeoseismicity and estimate recurrence intervals for large (>Mw7) earthquakes along the Cascadia Subduction Zone. Conventional models propose that upper slope failures are funneled into submarine canyons and develop into turbidity flows that are routed down-canyon to deep-water channel and fan systems. However, the sources and pathways of these turbidity flows are poorly constrained, leading to uncertainties in the connections between ground shaking, slope failure and deep-water turbidites. We examine the spatial distribution of sub

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13

Nelson, C. H., J. Gutiérrez Pastor, C. Goldfinger, and C. Escutia. "Great earthquakes along the Western United States continental margin: implications for hazards, stratigraphy and turbidite lithology." Natural Hazards and Earth System Sciences 12, no. 11 (2012): 3191–208. http://dx.doi.org/10.5194/nhess-12-3191-2012.

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Abstract. We summarize the importance of great earthquakes (Mw &amp;gtrsim; 8) for hazards, stratigraphy of basin floors, and turbidite lithology along the active tectonic continental margins of the Cascadia subduction zone and the northern San Andreas Transform Fault by utilizing studies of swath bathymetry visual core descriptions, grain size analysis, X-ray radiographs and physical properties. Recurrence times of Holocene turbidites as proxies for earthquakes on the Cascadia and northern California margins are analyzed using two methods: (1) radiometric dating (14C method), and (2) rela

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14

Kawagucci, Shinsuke, Tetsuya Miwa, Dhugal J. Lindsay, et al. "Deep-sea water displacement from a turbidity current induced by the Super Typhoon Hagibis." PeerJ 8 (December 9, 2020): e10429. http://dx.doi.org/10.7717/peerj.10429.

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Turbidity currents are the main drivers behind the transportation of terrestrial sediments to the deep sea, and turbidite deposits from such currents have been widely used in geological studies. Nevertheless, the contribution of turbidity currents to vertical displacement of seawater has rarely been discussed. This is partly because until recently, deep-sea turbidity currents have rarely been observed due to their unpredictable nature, being usually triggered by meteorological or geological events such as typhoons and earthquakes. Here, we report a direct observation of a deep-sea turbidity cu

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15

Starek, Dušan, Vladimír Šimo, Silvia Antolíková, and Tomáš Fuksi. "Turbidite sedimentology, biostratigraphy and paleoecology: A case study from the Oligocene Zuberec Fm. (Liptov Basin, Central Western Carpathians)." Geologica Carpathica 70, no. 4 (2019): 279–97. http://dx.doi.org/10.2478/geoca-2019-0016.

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Abstract Outcrops of a thick turbiditic succession are exposed on the northern bank of the Liptovská Mara reservoir near Liptovská Ondrašová and Ráztoky. The section consists of rhythmic, predominantly thin- to medium-bedded turbidites of the Rupelian age. Their biostratigraphy is based on the calcareous nannofossils. Facies associations of these deposits represent different components of depositional lobe deposits in the turbidity fan system, including mainly the lobe fringe and lobe distal fringe/inter-lobe facies associations and locally the medium bedded deposits of the lobe off-axis facie

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Baas, Jaco H., Niall D. Tracey, and Jeff Peakall. "Sole marks reveal deep-marine depositional process and environment: Implications for flow transformation and hybrid-event-bed models." Journal of Sedimentary Research 91, no. 9 (2021): 986–1009. http://dx.doi.org/10.2110/jsr.2020.104.

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ABSTRACT Deposits of sediment gravity flows in the Aberystwyth Grits Group (Silurian, west Wales, United Kingdom) display evidence that sole marks are suitable for reconstructing depositional processes and environments in deep-marine sedimentary successions. Based on drone imagery, 3D laser scanning, high-resolution sedimentary logging, and detailed descriptions of sole marks, an outcrop 1600 m long between the villages of Aberarth and Llannon was subdivided into seven lithological units, representing: a) mudstone-poor, coarse-grained and thick-bedded submarine channel fills, dominated by the

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Baas, Jaco H., Niall D. Tracey, and Jeff Peakall. "Sole marks reveal deep-marine depositional process and environment: Implications for flow transformation and hybrid-event-bed models." Journal of Sedimentary Research 91, no. 9 (2021): 986–1009. http://dx.doi.org/10.2110/jsr.2020.104.

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ABSTRACT Deposits of sediment gravity flows in the Aberystwyth Grits Group (Silurian, west Wales, United Kingdom) display evidence that sole marks are suitable for reconstructing depositional processes and environments in deep-marine sedimentary successions. Based on drone imagery, 3D laser scanning, high-resolution sedimentary logging, and detailed descriptions of sole marks, an outcrop 1600 m long between the villages of Aberarth and Llannon was subdivided into seven lithological units, representing: a) mudstone-poor, coarse-grained and thick-bedded submarine channel fills, dominated by the

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Suresh, N., and T. N. Bagati. "Ooid Turbidites from the Western Margin of the Bengal Fan Sediments." Journal Geological Society of India 50, no. 5 (1997): 619–27. http://dx.doi.org/10.17491/jgsi/1997/500511.

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Abstract Sedimentology, mineralogy and geochemistry of ooid sand beds in deep sea gravity cores (water depth &gt;2818 m) reveal that they were derived from continental shelf by turbidity currents. The presence of ooid turbidites at two different levels suggests two periods of turbidity current activity. The first activity probably took place during the Last Glacial Maximum in Late Pleistocene and the second activity prior to the stabilization of sea level in the Early Holocene.

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Jethra, Ravi. "Turbidity measurement." ISA Transactions 32, no. 4 (1993): 397–405. http://dx.doi.org/10.1016/0019-0578(93)90075-8.

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Sadar, Michael J. "Turbidity Revealed." Opflow 33, no. 1 (2007): 24–26. http://dx.doi.org/10.1002/j.1551-8701.2007.tb00007.x.

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OLIVERO, E. B., and M. I. LÓPEZ CABRERA. "HELMINTHOPSIS AND CYLINDRICHNUS ICHNOGUILDS FROM MIOCENE THIN-BEDDED TURBIDITES, TIERRA DEL FUEGO, ARGENTINA." Palaios 38, no. 9 (2023): 371–93. http://dx.doi.org/10.2110/palo.2022.058.

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Abstract Miocene thin-bedded turbidites from Tierra del Fuego record scarce graphoglyptids and two unusual ichnoguilds composed of diminutive elite trace fossils. The first, a monoichnospecific Cylindrichnus ichnoguild, consists of crowded, post-depositional burrows formed in surface sediments during the final phase of turbidite deposition. The second, a pre-depositional Helminthopsis ichnoguild, consists of dense aggregates of simple trails, mainly Helminthopsis and Helminthoidichnites, occupying a very shallow tier in organic-rich mud covering the sea floor prior to turbidite deposition. The

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Hanafie, Ahmad, Ilham Idrus, Wahyuddin Achmad, and Warits Al Qadri. "PENGARUH FLOKULASI MELALUI PENAMBAHAN ASAM FOSFAT (H3P04) TERHADAP KUALITAS GULA RAFINASI DI PT. MAKASSAR TENE." Journal Industrial Engineering and Management (JUST-ME) 2, no. 01 (2021): 31–38. http://dx.doi.org/10.47398/justme.v2i01.15.

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Mutu gula rafinasi merupakan salah satu hal yang sangat perlu di perhatikan, karena akan mempengaruhi kesehatan konsumen. Pada Penelitian ini bertujuan untuk meningkatkan kualitas gula rafinasi dengan cara mengurangi flok pada gula rafinasi dengan metode flokulasi menggunakan koagulan H3PO4 (asam fosfat). Untuk menentukan timbulnya flok pada gula rafinasi dengan penambahan bahan kimia yaitu H3PO4 (asam fosfat) dengan variabel pH (4, 5, dan 6) serta satu sampel tanpa penambahan asam fosfat dan di panaskan dengan suhu 800C selama 15 menit agar larutan gula cepat larut. Setelah larut dinginkan la

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Pouderoux, H., G. Lamarche, and J. N. Proust. "Building an 18 000-year-long paleo-earthquake record from detailed deep-sea turbidite characterisation in Poverty Bay, New Zealand." Natural Hazards and Earth System Sciences 12, no. 6 (2012): 2077–101. http://dx.doi.org/10.5194/nhess-12-2077-2012.

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Abstract. Two ~20 m-long sedimentary cores collected in two neighbouring mid-slope basins of the Paritu Turbidite System in Poverty Bay, east of New Zealand, show a high concentration of turbidites (5 to 6 turbidites per meter), interlaid with hemipelagites, tephras and a few debrites. Turbidites occur as both stacked and single, and exhibit a range of facies from muddy to sandy turbidites. The age of each turbidite is estimated using the statistical approach developed in the OxCal software from an exceptionally dense set of tephrochronology and radiocarbon ages (~1 age per meter). The age, to

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Hage, S., V. V. Galy, M. J. B. Cartigny, et al. "Efficient preservation of young terrestrial organic carbon in sandy turbidity-current deposits." Geology 48, no. 9 (2020): 882–87. http://dx.doi.org/10.1130/g47320.1.

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Abstract Burial of terrestrial biospheric particulate organic carbon in marine sediments removes CO2 from the atmosphere, regulating climate over geologic time scales. Rivers deliver terrestrial organic carbon to the sea, while turbidity currents transport river sediment further offshore. Previous studies have suggested that most organic carbon resides in muddy marine sediment. However, turbidity currents can carry a significant component of coarser sediment, which is commonly assumed to be organic carbon poor. Here, using data from a Canadian fjord, we show that young woody debris can be rapi

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Sibarani, Riama, and Ferry Febriansyah. "PERANCANGAN ALAT PENDETEKSI KEKERUHAN DAN PENGURASAN AIR." JURNAL LIMITS 20, no. 2 (2023): 23–30. http://dx.doi.org/10.59134/jlmt.v20i2.604.

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Kualitas air merupakan suatu faktor utama untuk pertumbuhan dan keberlangsungan hidup. Untuk menjaga kualitas air aqurium diperlukan suatu alat yang mampu mendeteksi tingkat kekeruhan dan menguras air yang kotor dan mengisi aquarium secara otomatis. Alat dirancang dengan menggunakan ESP32 dan Turbidity Sensor(TDS) yang berfungsi untuk mendeteksi tingkat kekeruhan air. Alat HC-SR04 digunakan untuk menentukan ketinggian volume air saat pengurasan dan pengisian air akuarium. Sensor Turbidty menampilkan informasitingkat kekeruhan air ditampilkan di layar LCD. Jika sensor Turbidity mendeteksi tingk

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Hesse, Reinhard, Sung Kwun Chough, and Allan Rakofsky. "The Northwest Atlantic Mid-Ocean Channel of the Labrador Sea. V. Sedimentology of a giant deep-sea channel." Canadian Journal of Earth Sciences 24, no. 8 (1987): 1595–624. http://dx.doi.org/10.1139/e87-155.

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The Northwest Atlantic Mid-Ocean Channel (NAMOC) is one of the largest deep-sea channels of the world's oceans. During the late Cenozoic glacial period, the channel played a major role in the depositional history of the Labrador Sea and northwest Atlantic in controlling sedimentation of a broad (approx. 500 m thick and 200 km wide) lens of turbidites. This sediment sequence interfingers laterally with the acoustically transparent pelagic and contourite facies found in the Labrador Basin. The meandering channel is a depositional–erosional feature formed by submarine mass flows, predominantly tu

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Ho, Viet Luan, Robert M. Dorrell, Gareth M. Keevil, Alan D. Burns, and William D. McCaffrey. "Scaling Analysis of Multipulsed Turbidity Current Evolution With Application to Turbidite Interpretation." Journal of Geophysical Research: Oceans 123, no. 5 (2018): 3668–84. http://dx.doi.org/10.1029/2017jc013463.

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Plink-Björklund, Piret, and Ron J. Steel. "Initiation of turbidity currents: outcrop evidence for Eocene hyperpycnal flow turbidites." Sedimentary Geology 165, no. 1-2 (2004): 29–52. http://dx.doi.org/10.1016/j.sedgeo.2003.10.013.

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Li, Yuting, and Peter D. Clift. "Controls on grain-size variability in the Holocene fill of the Indus Submarine Canyon." Journal of Sedimentary Research 93, no. 2 (2023): 71–87. http://dx.doi.org/10.2110/jsr.2022.038.

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ABSTRACT What processes control grain size and bed thickness in submarine canyon deposits? Erosive, shelf-cutting canyons contrast with accretionary basin-floor submarine fan accretionary channels because the former tightly constrain turbidity flows in deep channels. This study addresses such a deep-water depositional system in the Indus Submarine Canyon using a series of cores collected along the canyon. Grain-size analysis was conducted for turbidite and hemipelagic sediment deposited in the Holocene Indus Submarine Canyon mostly by diffuse, fine-grained turbidity currents and hemipelagic hy

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Noviasari, Linda, Asni Tafrikhatin, Juri Benedi, and Vicky Oby Syahputra. "Water Turbidity Detection Device Using Turbidity Sensor Based On Arduino Uno." Jurnal E-Komtek (Elektro-Komputer-Teknik) 8, no. 2 (2024): 438–44. https://doi.org/10.37339/e-komtek.v8i2.2219.

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A water turbidity detector using an Arduino Uno based turbidity sensor is a solution to measure water turbidity. The turbidity sensor functions to measure the level of water turbidity by detecting dissolved solid particles in it. The use of Arduino Uno as the main microcontroller, turbidity sensor to measure the level of turbidity and the results can be displayed clearly on the LCD. The main advantage of this tool is its ability to provide information about water turbidity. The integrated LED and Buzzer also provide notification if the water turbidity level has been set. In addition, the simpl

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Heerema, Catharina J., Matthieu J. B. Cartigny, Ricardo Silva Jacinto, Stephen M. Simmons, Ronan Apprioual, and Peter J. Talling. "How distinctive are flood-triggered turbidity currents?" Journal of Sedimentary Research 92, no. 1 (2022): 1–11. http://dx.doi.org/10.2110/jsr.2020.168.

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ABSTRACT Turbidity currents triggered at river mouths form an important highway for sediment, organic carbon, and nutrients to the deep sea. Consequently, it has been proposed that the deposits of these flood-triggered turbidity currents provide important long-term records of past river floods, continental erosion, and climate. Various depositional models have been suggested to identify river-flood-triggered turbidite deposits, which are largely based on the assumption that a characteristic velocity structure of the flood-triggered turbidity current is preserved as a recognizable vertical grai

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Gregory, John. "Turbidity and beyond." Filtration & Separation 35, no. 1 (1998): 63–67. http://dx.doi.org/10.1016/s0015-1882(97)83117-5.

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Gregory, J. "Turbidity and beyond." Filtration & Separation 35, no. 1 (1998): 62. http://dx.doi.org/10.1016/s0015-1882(98)90665-6.

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Saiyar, Hafdiarsya, and Mohammad Noviansyah. "IDENTIFICATION OF WATER TURBIDITY WITH TURBIDITY SENSOR BASED ON ARDUINO." Jurnal Riset Informatika 3, no. 4 (2021): 395–400. http://dx.doi.org/10.34288/jri.v3i4.277.

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Water is an important need for all living things, especially humans. Humans need water with quality that meets the physical, microbiological, chemical, and radiological requirements contained in the mandatory and additional parameters. The selection of these parameters is very important to meet the requirements of good water, namely tasteless, odorless, and colorless. Meanwhile, there are three parameters used for water identification, namely pH parameters, turbidity levels, and temperature parameters. From these problems, the authors examine the detection of water quality, especially water tu

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Grenier, J. C., A. De La Casinière, and T. Cabot. "Atmospheric Turbidity Analyzed by Means of Standardized Linke's Turbidity Factor." Journal of Applied Meteorology 34, no. 6 (1995): 1449–58. http://dx.doi.org/10.1175/1520-0450(1995)034<1449:atabmo>2.0.co;2.

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Ercilla, Gemma, Russell B. Wynn, Belén Alonso, and Jesús Baraza. "Initiation and evolution of turbidity current sediment waves in the Magdalena turbidite system." Marine Geology 192, no. 1-3 (2002): 153–69. http://dx.doi.org/10.1016/s0025-3227(02)00553-4.

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Cantero, Mariano I., Alessandro Cantelli, Carlos Pirmez, et al. "Emplacement of massive turbidites linked to extinction of turbulence in turbidity currents." Nature Geoscience 5, no. 1 (2011): 42–45. http://dx.doi.org/10.1038/ngeo1320.

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Völker, David, Thomas Reichel, Michael Wiedicke, and Christoph Heubeck. "Turbidites deposited on Southern Central Chilean seamounts: Evidence for energetic turbidity currents." Marine Geology 251, no. 1-2 (2008): 15–31. http://dx.doi.org/10.1016/j.margeo.2008.01.008.

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Hall, Damien, Ran Zhao, Ian Dehlsen, et al. "Protein aggregate turbidity: Simulation of turbidity profiles for mixed-aggregation reactions." Analytical Biochemistry 498 (April 2016): 78–94. http://dx.doi.org/10.1016/j.ab.2015.11.021.

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Annadurai, Gurusamy, S. S. Sung, and Duu-Jong Lee. "Simultaneous removal of turbidity and humic acid from high turbidity stormwater." Advances in Environmental Research 8, no. 3-4 (2004): 713–25. http://dx.doi.org/10.1016/s1093-0191(03)00043-1.

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Nury, Dennis, Rifqi Sufra, Mega Tiara, Siti Aisyah Rahimah Aulia, Siti Aisyah Rahimah Aulia, and Muhammad Zulfikar Luthfi. "Evaluasi Dosing Flokulan terhadap Waktu Pengendapan Juice pada Single Tray Clarifier di PT. Pemukasakti Manisindah." ISTA Online Technologi Journal 4, no. 2 (2023): 18–27. http://dx.doi.org/10.62702/ion.v4i2.88.

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Abstrak Salah satu parameter untuk mendapatkan gula sesuai standar SNI adalah kemurnian nira. Nira merupakan cairan hasil ekstraksi tebu. Nira akan dipisahkan dari kotoran menjadi nira jernih dengan ditambahkan flokulan. Konsentrasi flokulan juga sangat berpengaruh terhadap pengendapan nira. Penelitian ini bertujuan menentukan dosis flokulan yang efektif untuk meningkatkan laju pengendapan kotoran nira dan mengetahui dosis flokulan yang dapat mempengaruhi kualitas clear juice atau nira encer. Pengujian yang dilakukan meliputi pengujian jar test, pengukuran turbiditas, pH dan pengamatan warna.

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Juliantara, I. Putu Eka, Lutfi Suhendra, and Anak Agung Made Dewi Anggreni. "Karakteristik Mikroemulsi Minyak Atsiri Sirih (Piper betle L) Pada Lama Pengadukan Dan Suhu." JURNAL REKAYASA DAN MANAJEMEN AGROINDUSTRI 11, no. 3 (2023): 341. http://dx.doi.org/10.24843/jrma.2023.v11.i03.p02.

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The betel plant (Piper betle L) is a plant that has the ability as an antifungal, antimicrobial and antioxidant. In order to make betel essential oil more efficient to use, betel essential oil is made into a microemulsion. The purpose of this study was to determine the effect of stirring time and temperature on the characteristics of betel essential oil microemulsions and to determine the best stirring time and temperature to produce betel essential oil microemulsion characteristics. This experiment used a randomized block design (RBD) using two factors, namely mixing time and temperature. The

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Larsen, P. H. "Soft sediment deformation structures in Silurian turbidites from North Greenland." Bulletin of the Geological Society of Denmark 35 (October 29, 1986): 19–23. http://dx.doi.org/10.37570/bgsd-1986-35-03.

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Turbidite beds in the Silurian turbidite sequence, North Greenland, show soft sediment deformation structures suggesting that the structureless (in respect of traction structures) sandstones divisions of the turbidites were deposited by direct suspension sedimentation from high-density flows. The deposits may have resulted from multiple successive depositional events within the same turbidity flow. Reworking and shear- ing of the newly formed loosely packed high-density suspension deposits caused by the still moving flow above create secondary soft sediment deformation structures which may

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Ichikawa, Kenta, Kenta Iitani, Gentaro Kawase, et al. "Mouthguard-Type Wearable Sensor for Monitoring Salivary Turbidity to Assess Oral Hygiene." Sensors 24, no. 5 (2024): 1436. http://dx.doi.org/10.3390/s24051436.

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Salivary turbidity is a promising indicator for evaluating oral hygiene. This study proposed a wearable mouthguard-type sensor for continuous and unconstrained measurement of salivary turbidity. The sensor evaluated turbidity by measuring the light transmittance of saliva with an LED and a phototransistor sealed inside a double-layered mouthguard. The sensor was also embedded with a Bluetooth wireless module, enabling the wireless measurement of turbidity. The mouthguard materials (polyethylene terephthalate-glycol and ethylene-vinyl acetate) and the wavelength of the LED (405 nm) were experim

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Vrbanac, Boris, Josipa Velić, and Tomislav Malvić. "Sedimentation of deep-water turbidites in the SW part of the Pannonian Basin." Geologica Carpathica 61, no. 1 (2010): 55–69. http://dx.doi.org/10.2478/v10096-010-0001-8.

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Sedimentation of deep-water turbidites in the SW part of the Pannonian BasinThe Sava Depression and the Bjelovar Subdepression belong to the SW margin of the Pannonian Basin System, which was part of the Central Paratethys during the Pannonian period. Upper Pannonian deposits of the Ivanic-Grad Formation in the Sava Depression include several lithostratigraphic members such as Iva and Okoli Sandstone Member or their lateral equivalents, the Zagreb Member and Lipovac Marlstone Member. Their total thickness in the deepest part of the Sava Depression reaches up to 800 meters, while it is 100-200

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Voichick, Nicholas, David J. Topping, and Ronald E. Griffiths. "Technical note: False low turbidity readings from optical probes during high suspended-sediment concentrations." Hydrology and Earth System Sciences 22, no. 3 (2018): 1767–73. http://dx.doi.org/10.5194/hess-22-1767-2018.

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Abstract. Turbidity, a measure of water clarity, is monitored for a variety of purposes including (1) to help determine whether water is safe to drink, (2) to establish background conditions of lakes and rivers and detect pollution caused by construction projects and stormwater discharge, (3) to study sediment transport in rivers and erosion in catchments, (4) to manage siltation of water reservoirs, and (5) to establish connections with aquatic biological properties, such as primary production and predator–prey interactions. Turbidity is typically measured with an optical probe that detects l

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Lange Jensen, Lasse, Thomas Bjørn, Andreas Hein Korsgaard, Cino Pertoldi, and Niels Madsen. "Influence of Turbidity on Foraging Behaviour in Three-Spined Sticklebacks (Gasterosteus aculeatus)." Fishes 8, no. 12 (2023): 609. http://dx.doi.org/10.3390/fishes8120609.

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Anthropogenic activities increase turbidity in coastal marine environments globally, and turbidity is particularly caused by eutrophication. Turbidity is a measurement of the scattering and absorption of light by suspended matter in water. An increase in turbidity influences visual predators and affects community structures and whole ecosystems. The three-spined stickleback (Gasterosteus aculeatus) is a widespread species in the northern hemispheric Pacific and Atlantic oceans. It is a visual predator and, therefore, a very well-suited species for studying the effects of increasing turbidity o

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SoneyeArogundade, Olanrewaju Olukemi, and Bernhard Rappenglück. "The Variation in Atmospheric Turbidity over a Tropical Site in Nigeria and Its Relation to Climate Drivers." Atmosphere 15, no. 3 (2024): 367. http://dx.doi.org/10.3390/atmos15030367.

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Atmospheric turbidity exhibits substantial spatial–temporal variability due to factors such as aerosol emissions, seasonal changes, meteorology, and air mass transport. Investigating atmospheric turbidity is crucial for climatology, meteorology, and atmospheric pollution. This study investigates the variation in atmospheric turbidity over a tropical location in Nigeria, utilizing the Ångström exponent (α), the turbidity coefficient (β), the Linke turbidity factor (TL), the Ångström turbidity coefficient (βEST), the Unsworth–Monteith turbidity coefficient (KAUM), and the Schüepp turbidity coeff

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Shen, Ming, Siyuan Wang, Yingkui Li, Maofeng Tang, and Yuanxu Ma. "Pattern of Turbidity Change in the Middle Reaches of the Yarlung Zangbo River, Southern Tibetan Plateau, from 2007 to 2017." Remote Sensing 13, no. 2 (2021): 182. http://dx.doi.org/10.3390/rs13020182.

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Turbidity is an important indicator of riverine conditions, especially in a fragile environment such as the Tibetan Plateau. Remote sensing, with the advantages of large-scale observations, has been widely applied to monitor turbidity change in lakes and rivers; however, few studies have focused on turbidity change of rivers on the Tibetan Plateau. We investigated the pattern of turbidity change in the middle reaches of the Yarlung Zangbo River, southern Tibetan Plateau, based on multispectral satellite imagery and in situ measurements. We developed empirical models from in situ measured water

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Shen, Ming, Siyuan Wang, Yingkui Li, Maofeng Tang, and Yuanxu Ma. "Pattern of Turbidity Change in the Middle Reaches of the Yarlung Zangbo River, Southern Tibetan Plateau, from 2007 to 2017." Remote Sensing 13, no. 2 (2021): 182. http://dx.doi.org/10.3390/rs13020182.

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Turbidity is an important indicator of riverine conditions, especially in a fragile environment such as the Tibetan Plateau. Remote sensing, with the advantages of large-scale observations, has been widely applied to monitor turbidity change in lakes and rivers; however, few studies have focused on turbidity change of rivers on the Tibetan Plateau. We investigated the pattern of turbidity change in the middle reaches of the Yarlung Zangbo River, southern Tibetan Plateau, based on multispectral satellite imagery and in situ measurements. We developed empirical models from in situ measured water

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