Artículos de revistas: "Natron"

1

Marsha-Ann Watson. "Natron Energy". C&EN Global Enterprise 98, n.º 44 (16 de noviembre de 2020): 40–41. http://dx.doi.org/10.1021/cen-09844-cover8.

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2

Pauls, T. "Natron Trade, 2000 B.C." Science 280, n.º 5362 (17 de abril de 1998): 359e—359. http://dx.doi.org/10.1126/science.280.5362.359e.

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3

Manega, Paul y Sophie Bieda. "Modern sediments of Lake Natron, Tanzania. Sédimentation récente du lac Natron, Tanzanie". Sciences Géologiques. Bulletin 40, n.º 1 (1987): 83–95. http://dx.doi.org/10.3406/sgeol.1987.1752.

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4

Mturi, Amini A. "The archeological sites of Lake Natron (Tanzania). Sites archéologiques du lac Natron (Tanzanie)". Sciences Géologiques. Bulletin 40, n.º 1 (1987): 209–15. http://dx.doi.org/10.3406/sgeol.1987.1761.

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5

Borchers, Moritz. "AML: Rezidivprophylaxe mit Natron nach HSZT". InFo Hämatologie + Onkologie 23, n.º 12 (diciembre de 2020): 44. http://dx.doi.org/10.1007/s15004-020-8340-9.

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6

Fordos, M. J. y A. Gélis. "Einwirkung von Goldchlorid auf unterschwefligsaures Natron". Journal für Praktische Chemie 35, n.º 1 (8 de noviembre de 2004): 321–28. http://dx.doi.org/10.1002/prac.18450350149.

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7

Celestina Adebimpe Ojo, Makanju Dehinde Awogbenja, Eunice Adigizi y Tomiwa Johnson Oyedokun. "Histological and proximate analysis of ash produced from sesame, palm fruit and Parkia on albino rats". International Journal of Biological and Pharmaceutical Sciences Archive 2, n.º 2 (30 de noviembre de 2021): 026–30. http://dx.doi.org/10.53771/ijbpsa.2021.2.2.0077.

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The customary puerperal usage of Natron consumption has been identified as one of the risk factors in the cause of high blood pressure in human as well as kidney diseases and abortion in early pregnancies in female. This study was done to determine the effect of Natron and other Natron alternatives on the histology of kidney and liver in male Wistar Albino rats Twenty-five Wistar albino rats of the same sexes (male) weighing 100- 140 kg body weights were used and were divided into five groups. Group 1, 2, 3 and 4 were fed with feed mixed with natron powder, feed mixed with wood ash, feed mixed with sesame ash, feed mixed with palm fruit bunch ash respectively, while group 6 served as a normal control (fed with plain feed). The animals were kept in plastic cages, allowed to acclimatize for two weeks before the commencement of the experiment. They were fed with pelletized growers’ feed (Vital feed) and were allowed access to water. The rats were fed with 25kg of feeds for 12 days to allow them stabilized and recover from stress. Then the rats were fed with the pelletized feed for four weeks to all the groups. The animals were anaesthetized with chloroform vapour after 4 weeks and blood samples were collected through cardiac puncture into labeled tubes for electrolyte analyses. The labeled centrifuge tubes were allowed to stand for 30 minutes to clot and centrifuged at 4000 g for 10mm and the serum obtained was pipette into labeled tubes. The organs were subjected to histology. The liver tissues were embedded in paraffin wax, sectioned at 5μm and stained by hematoxylin and eosin. Proximate analysis showed that natron, palm bunch ash, sesame stem ash, and parkia wood ash had crude protein values of 0.03%, 0.05%, 0.07%, and 0.09% respectively. Fat and fiber were not present in both Natron and its alternatives. The appreciable amount of ash content in the food additives indicated good mineral preservation capacity. Parkia wood ash may contain toxic chemical substances that may affect the kidney and liver.

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8

Fritz, Bertrand, Marie-Paul Zins-Pawlas y Moncef Gueddari. "Geochemistry of silica-rich brines from Lake Natron (Tanzania). Géochimie des saumures riches en silice du lac Natron (Tanzanie)". Sciences Géologiques. Bulletin 40, n.º 1 (1987): 97–110. http://dx.doi.org/10.3406/sgeol.1987.1753.

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9

Hillaire-Marcel, Claude. "Hydrologie isotopique des lacs Magadi (Kenya) et Natron (Tanzanie). Isotopic hydrology of the lakes Magadi (Kenya ) and Natron (Tanzania )". Sciences Géologiques. Bulletin 40, n.º 1 (1987): 111–20. http://dx.doi.org/10.3406/sgeol.1987.1754.

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10

Tamura, Tomomi y Katsuhiko Oga. "Archaeometrical investigation of natron glass excavated in Japan". Microchemical Journal 126 (mayo de 2016): 7–17. http://dx.doi.org/10.1016/j.microc.2015.11.029.

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11

Torre, Ignacio de la, Rafael Mora y Jorge Martínez-Moreno. "The early Acheulean in Peninj (Lake Natron, Tanzania)". Journal of Anthropological Archaeology 27, n.º 2 (junio de 2008): 244–64. http://dx.doi.org/10.1016/j.jaa.2007.12.001.

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12

Suner, Fikret, Ö. Işik Ece, Fazlı Çoban y Fahri Esenli. "Occurrence and properties of natron in the Miocene lacustrine Beypazari basin, Turkey". Neues Jahrbuch für Mineralogie - Monatshefte 2003, n.º 1 (16 de enero de 2003): 31–48. http://dx.doi.org/10.1127/0028-3649/2003/2003-0031.

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13

Saguí, Lucia. "GLASS IN LATE ANTIQUITY: THE CONTINUITY OF TECHNOLOGY AND SOURCES OF SUPPLY". Late Antique Archaeology 4, n.º 1 (2008): 211–31. http://dx.doi.org/10.1163/22134522-90000089.

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Scientific research and a series of important archaeological discoveries in recent years have opened up new perspectives on the study of ancient glass. Glass production seems to have been organised on a hierarchical basis. The primary workshops, mainly concentrated on the Syro-Palestinian coast, prepared the raw material by fusing sand from the river Belus with natron from Egypt. The product was then sent in blocks to all secondary workshops, the organisation of which was less elaborate. Here work was limited to re-fusing material that had already been worked. The widespread commercial movement of raw glass from East to West seems to have only come to a halt in the 9th c., when the export of natron from Egypt stopped. Consequently, a different flux was used, which was incompatible with the oriental sand. The adoption of local raw materials in the place of natron meant that the management of the entire production cycle became gradually autonomous, at different speeds and in different ways, during the course of the Middle Ages.

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14

Geraads, Denis. "La faune des dépôts pléistocènes de l'Ouest du lac Natron (Tanzanie) ; interprétation biostratigraphique. The Pleistocene fauna from West Natron (Tanzania) ; biostratigraphic interpretation". Sciences Géologiques. Bulletin 40, n.º 1 (1987): 167–84. http://dx.doi.org/10.3406/sgeol.1987.1758.

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15

Thouveny, N. y M. Taieb. "Preliminary magnetostratigraphic record of Pleistocene deposits, Lake Natron Basin, Tanzania". Geological Society, London, Special Publications 25, n.º 1 (1986): 331–36. http://dx.doi.org/10.1144/gsl.sp.1986.025.01.27.

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16

Dotsika, E., D. Poutoukis, I. Tzavidopoulos, Y. Maniatis, D. Ignatiadou y B. Raco. "A natron source at Pikrolimni Lake in Greece? Geochemical evidence". Journal of Geochemical Exploration 103, n.º 2-3 (noviembre de 2009): 133–43. http://dx.doi.org/10.1016/j.gexplo.2009.08.003.

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17

Edwards, Howell G. M., Katherine J. Currie, Hassan R. H. Ali, Susana E. Jorge Villar, A. Rosalie David y John Denton. "Raman spectroscopy of natron: shedding light on ancient Egyptian mummification". Analytical and Bioanalytical Chemistry 388, n.º 3 (3 de abril de 2007): 683–89. http://dx.doi.org/10.1007/s00216-007-1249-4.

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18

EBINGER, C., Y. POUDJOM DJOMANI, E. MBEDE, A. FOSTER y J. B. DAWSON. "Rifting Archaean lithosphere: the Eyasi-Manyara-Natron rifts, East Africa". Journal of the Geological Society 154, n.º 6 (noviembre de 1997): 947–60. http://dx.doi.org/10.1144/gsjgs.154.6.0947.

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19

Finkenberger, Johannes, Anika Deinhardt, Johanna Kron, Martin Kilo, Thomas Ballweg y Jürgen Meinhardt. "Elektrochemisches Verhalten von Elektrodenmaterialien in Schmelzen von Kalk-Natron-Silicatgläsern". Chemie Ingenieur Technik 88, n.º 4 (17 de septiembre de 2015): 469–74. http://dx.doi.org/10.1002/cite.201500018.

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20

Hilcken, Jonas, Kaja Boxheimer, Jens Schneider, Johann-Dietrich Wörner y Johannes Franz. "Untersuchung der zyklischen Ermüdung von thermisch vorgespanntem Kalk-Natron-Silikatglas". Stahlbau 83, S1 (abril de 2014): 253–66. http://dx.doi.org/10.1002/stab.201490064.

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21

Браше, Жюльен y Юдит Шиле. "Политэкономия натрона в регионе Борку (Республика Чад)". Антропологии/Anthropologies, n.º 1 (12 de noviembre de 2021): 62–77. http://dx.doi.org/10.33876/2782-3423/2021-1/62-77.

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Экспорт натрона с главной кустарной выработки в регионе Борку облагается налогом совместно вождем племенного клана и правительственным чиновником. История формирования этого не-устойчивого соглашения показывает, что “вожди” и “государство” нуждаются друг в друге для утверждения своего рода суверенитета над этим регионом. Частный случай налогообложения натрона является показательным для понимания государственного устройства Республики Чад в целом, с его дублированием официальных административных структур традиционными и системой взаимодействия локального и национального уровней политической власти. Статья основана на результатах восьмимесячного полевого исследования обоих авторов на севере Чада в 2012 г., а также на работе в местных и национальных архивах. Natron is mined by hand in open-air mines throughout the Chadian Sahara. In the main mine in Borkou, it is taxed by a local “traditional chief” as well as by a government representative. The way this fiscal arrangement came about historically shows how “traditional chiefs” and “the state” need each other in order to claim a particular and particularly restricted kind of sovereignty in the region. This is true of the Chadian state more generally, marked by a doubling up of “official” and “traditional” administrative hierarchies, and a close but rarely simple articulation of the local and the national level.

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22

Plasman, Matthieu, Sophie Hautot, Pascal Tarits, Stéphanie Gautier, Christel Tiberi, Bernard Le Gall, Khalfan Mtelela y Remigius Gama. "Lithospheric Structure of a Transitional Magmatic to Amagmatic Continental Rift System—Insights from Magnetotelluric and Local Tomography Studies in the North Tanzanian Divergence, East African Rift". Geosciences 9, n.º 11 (29 de octubre de 2019): 462. http://dx.doi.org/10.3390/geosciences9110462.

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Continental break-up is controlled by several parameters and processes (rheology, inherited structures, magmatism, etc). Their impact, chronology and interactions are still poorly known and debated, particularly when rifting interacts with cratons. In order to better understand the rifting initiation in a cratonic lithosphere, we analysed 22 magnetotelluric (MT) soundings collected along two East-West profiles in two different rift segments of the North Tanzanian Divergence. The North Tanzanian Divergence, where the East African Rift is at its earliest stage, is a remarkable example of the transition between magmatic to amagmatic rifting with two clearly identified segments. Only separated by a hundred kilometers, these segments, Natron (North) and Manyara (South), display contrasted morphological (wide versus narrow), volcanic (many versus a few edifices) and seismic (shallow versus deep activity) signatures. Magnetotelluric profiles across the two segments were inverted with a three-dimensional approach and supplied the resistive structure of the upper lithosphere (down to about 70 km). The Natron segment has a rather conductive lithosphere containing several resistive features (Proterozoic Belt), whereas the Manyara segment displays highly resistive blocks probably of cratonic nature encompassing a conductive structure under the axial valley. The joint interpretation of these models with recent local and regional seismological studies highlights totally different structures and processes involved in the two segments of the North Tanzanian Divergence. We identified contrasted CO2 content, magma upwelling or trapping, in depth regarding the Manyara or the Natron branch and the influence of inherited cratonic structures in the rifting dynamics.

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23

Icole, Michel, Maurice Taieb, Guy Périnet, Paul Manega y Christian Robert. "Minéralogie des sédiments du groupe Peninj (lac Natron, Tanzanie). Reconstitution des paléoenvironnements lacustres. Mineralogical records of the Peninj Group (Lake Natron, Tanzania). Lacustrine paleoenvironment implications". Sciences Géologiques. Bulletin 40, n.º 1 (1987): 71–82. http://dx.doi.org/10.3406/sgeol.1987.1751.

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24

Casanova, Joel. "Stromatolites et hauts niveaux lacustres pléistocènes du bassin Natron-Magadi (Tanzanie-Kenya). Pleistocene stromatolites and high lake levels of the Natron-Magadi basin (Tanzania-Kenya)". Sciences Géologiques. Bulletin 40, n.º 1 (1987): 135–53. http://dx.doi.org/10.3406/sgeol.1987.1756.

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25

Denys, Christiane. "Micromammals from the West Natron Pleistocene deposits (Tanzania). Biostratigraphy and paleoecology. Les micromammifères des dépôts pléistocènes de l'Ouest du lac Natron (Tanzanie). Biostratigraphie et paléoécologie". Sciences Géologiques. Bulletin 40, n.º 1 (1987): 185–201. http://dx.doi.org/10.3406/sgeol.1987.1759.

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26

Busatlic, Ilhan, Sefkija Botonjic, Azra Halilovic, Nadira Busatlic y Amna Karic. "Positive examples of wastewater treatment effectiveness in ‘Natron-Hayat’ Maglaj factory". Reciklaza i odrzivi razvoj 10, n.º 1 (2017): 23–30. http://dx.doi.org/10.5937/ror1701023b.

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27

Aly, Mohamed. "ECOLOGICAL STUDIES ON PHYTOPLANKTON IN CLOSED LAKES OF WADI-EL-NATRON". Egyptian Journal of Phycology 1, n.º 1 (1 de noviembre de 2000): 203–10. http://dx.doi.org/10.21608/egyjs.2000.113255.

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28

Arrott, A. R. "Ueber eine Classe von Doppelsalzen, welche Natron, Magnesia und Schwefelsäure enthalten". Journal für Praktische Chemie 33, n.º 1 (8 de noviembre de 2004): 372–74. http://dx.doi.org/10.1002/prac.18440330149.

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29

Vincens, Annie y Joel Casanova. "Modern background of Natron-Magadi basin (Tanzania-Kenya) : physiography, climate, hydrology and vegetation. Contexte actuel du bassin Natron-Magadi (Tanzanie-Kenya) : physiographie, climat, hydrologie et végétation". Sciences Géologiques. Bulletin 40, n.º 1 (1987): 9–21. http://dx.doi.org/10.3406/sgeol.1987.1747.

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30

Abdallah, Edista A., Charles H. Kasanzu, Crispin P. Kinabo, Akira Imai y Mike J. Butler. "Constraining the Origin and Age of the Thermal and Cold Water in the Lake Natron Basin, Northern Tanzania". Tanzania Journal of Science 48, n.º 4 (30 de diciembre de 2022): 804–15. http://dx.doi.org/10.4314/tjs.v48i4.8.

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Springs on the eastern and western shores of Lake Natron Basin (LNB), located within the eastern branch of the East Africa Rift System (EARS) in Northern Tanzania had a discharge temperature that ranged between 34.0 °C and 51.2 °C, while the pH varied from 8.0 to 10.7. The electrical conductivity (EC) ranged between 5,007 µS/cm and 49,200 µS/cm. Cold waters had a temperature of 31.9 °C to 32.5 °C, while the pH ranged between 8.0 and 8.3, and the EC ranged between 1,401 µS/cm and 3,806 µS/cm. The stable isotope composition varied between -2.4 ‰ and -5.3 ‰ for δ18O, and -15.5 ‰ to -29.3 ‰ for δ2H. The isotopic composition of thermal and cold water of LNB indicates a significant contribution of meteoric water in the recharge of the hydrothermal system. However, thermal water is affected by evaporation, water-rock interaction, carbon dioxide (CO2) exchange and condensation processes. Tritium analysis indicated that the spring water in the LNB hydrothermal system has a residence time of more than 50 years. Keywords: thermal water; Lake Natron Basin; stable isotopes; springs.

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31

Brachet, Julien y Judith Scheele. "Fiscalit� marginale sur mesure. L��conomie politique du natron au Borkou, Tchad". Politique africaine 151, n.º 3 (2018): 39. http://dx.doi.org/10.3917/polaf.151.0039.

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32

Kadigi, Reuben M. J., Ken Mwathe, Adam Dutton, Japhet Kashaigili y Freddy Kilima. "Soda Ash Mining in Lake Natron: A Reap or Ruin for Tanzania?" Journal of Environmental Conservation Research 2, n.º 2 (2014): 37. http://dx.doi.org/10.12966/jecr.05.01.2014.

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33

Arcones-Pascual, Gustavo, Francisco Hernández-Olivares y Alberto Sepulcre-Aguilar. "Comparative properties of a lime mortar with different metakaolin and natron additions". Construction and Building Materials 114 (julio de 2016): 747–54. http://dx.doi.org/10.1016/j.conbuildmat.2016.03.170.

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34

Josset, Patrick. "Emplois thérapeutiques du natron dans l'Egypte antique et le monde gréco-romain". Revue d'histoire de la pharmacie 84, n.º 311 (1996): 385–96. http://dx.doi.org/10.3406/pharm.1996.4824.

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35

Baryshev, Alexander. "Advective structures of the bottom of lake Natron and its surroundings (Tanzania)". Ores and metals, n.º 3 (15 de noviembre de 2022): 101–9. http://dx.doi.org/10.47765/0869-5997-2022-10019.

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In this study we consider the features of the development of weakly lithified bottom sediments and the general structure of lake Natron against the background of its seasonal drying and watering. This study takes into account the laws of advection and the periodic placement of cellular zonal advective structures in space. The consedimentary structures in the lake sediments demonstrate the conditions for the formation of sodic ores and their positions. Provided space and aerial photographs depict unique genetic information about the evolution of geochemistry and the development of bottom morphology during sedimentation. This includes the presence of two sources that feed the lake - river and mud eruptions of the adjacent Oldoinyo-Lengai volcano, supposedly the only one on Earth that erupts carbonatite lavas. The combination of two sources and two processes leads to the development of an epimagmatic phreatic-hydrothermal recycling system. In it, the masses of the lake penetrate through fissure structures into the suprafocal space of the volcano, providing mud volcanism with solutions of soda masses containing organic matter of sediments. Volcanic soda eruptions are not carbonatite lavas. The morphological similarities and differences of structures are shown - small craters on the bottom of the lake, associated with the advection of thin layers of sedimentary material; large craters located nearby among volcanic strata along the shores of the lake; and both subsidence calderas and explosion calderas associated with magmatic and mud types of volcanism in the setting of strike-slip transtension.

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36

de la Torre Sáinz, Ignacio y Manuel Domínguez Rodrigo. "Historia de las intervenciones en Peninj (lago Natron, Tanzania), en el contexto de la arqueología del Plio-pleistoceno africano". SPAL. Revista de Prehistoria y Arqueología de la Universidad de Sevilla, n.º 10 (2001): 123–34. http://dx.doi.org/10.12795/spal.2001.i10.06.

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37

Liu, Tingting, David L. Bish, Richard A. Socki, Ralph P. Harvey y Eric Tonui. "Mineralogy and formation of evaporite deposits from the Lewis Cliff ice tongue, Antarctica". Antarctic Science 27, n.º 1 (5 de septiembre de 2014): 73–84. http://dx.doi.org/10.1017/s0954102014000406.

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AbstractThe mineralogy of evaporites from the Lewis Cliff ice tongue (LCIT), Antarctica, and their mineral stabilities and transformation behaviours under different temperature and relative humidity (RH) conditions have been evaluated to elucidate formation mechanism(s). A variety of sodium (Na)-rich evaporite minerals were documented using RH-controlled powder X-ray diffraction (XRD) methods including Na-sulfates (mirabilite and thenardite), Na-carbonate/bicarbonates (nahcolite, occasional trona and natron) and Na-borates (qilianshanite and borax). Mirabilite begins to dehydrate to thenardite, and natron to trona and natrite when exposed to room temperature, even when maintained at RH values similar to those measured at the LCIT (50–70%). The boron-mineral qilianshanite was discovered for the first time in Antarctica within the evaporite mounds. The mirabilite-rich mounds are deduced to have formed via a freezing/sublimation process that occurred in glacial or subglacial bodies of water supplied by glacial tills containing microbially oxidized sulfate ions. The needle-like nahcolite crystals growing on the exteriors of the mounds suggest a dissolution/precipitation process involving atmospheric CO2 and water. The co-existence of nahcolite and boron-bearing minerals indicates the presence of a Na+-, HCO3-- and boron-bearing alkaline brine, which produces qilianshanite as a secondary mineral by reaction of nahcolite and borax in atmospheric CO2 and H2O.

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38

Saidu, Yusuf, Rihanat Olawumi Olaosebikan, Suleiman Ahmed Isa, Ibrahim Malami y Suleiman Alhaji Muhammad. "Effect of natron administration on the antioxidant status and lipid profile of rats". Journal of Food Science 85, n.º 11 (30 de septiembre de 2020): 4033–38. http://dx.doi.org/10.1111/1750-3841.15480.

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39

Bosch, Pim L. F. van den, Marc Fortuny-Picornell y Albert J. H. Janssen. "Effects of Methanethiol on the Biological Oxidation of Sulfide at Natron-Alkaline Conditions". Environmental Science & Technology 43, n.º 2 (15 de enero de 2009): 453–59. http://dx.doi.org/10.1021/es801894p.

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40

Jackson, C. M., S. Paynter, M. D. Nenna y P. Degryse. "Glassmaking using natron from el-Barnugi (Egypt); Pliny and the Roman glass industry". Archaeological and Anthropological Sciences 10, n.º 5 (19 de diciembre de 2016): 1179–91. http://dx.doi.org/10.1007/s12520-016-0447-4.

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41

Völker, K., K. H. Zum Gahr, W. Pannhorst y W. Beier. "Untersuchungen zur Haftreibung zwischen faserverstärktem Borosilicatglas und Kalk-Natron-Glas bei erhöhten Temperaturen". Materialwissenschaft und Werkstofftechnik 30, n.º 1 (enero de 1999): 5–13. http://dx.doi.org/10.1002/(sici)1521-4052(199901)30:1<5::aid-mawe5>3.0.co;2-f.

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42

Kaufman, Aaron, Mordeckai Margaritz, Michael Paul, Claude Hillaire-Marcel, George Hollos, Elisabetta Boaretto y Maurice Taieb. "The 36C1 ages of the brines in the Magadi-Natron basin, East Africa". Geochimica et Cosmochimica Acta 54, n.º 10 (octubre de 1990): 2827–33. http://dx.doi.org/10.1016/0016-7037(90)90017-f.

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43

Penny, F. "Ueber die Wirkung von Salpetersäure auf chlor-, jod- und bromsaures Kali und Natron". Journal für Praktische Chemie 23, n.º 1 (8 de noviembre de 2004): 296–98. http://dx.doi.org/10.1002/prac.18410230137.

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44

Moubasher, AH. "Ramophialophora chlamydospora, a new species from an alkaline lake of Wadi-El-Natron, Egypt". Asian Journal of Mycology 2, n.º 1 (2019): 110–17. http://dx.doi.org/10.5943/ajom/2/1/5.

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45

Mattsson, Hannes B. y Barbara A. Tripoli. "Depositional characteristics and volcanic landforms in the Lake Natron–Engaruka monogenetic field, northern Tanzania". Journal of Volcanology and Geothermal Research 203, n.º 1-2 (junio de 2011): 23–34. http://dx.doi.org/10.1016/j.jvolgeores.2011.04.010.

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46

Scott, Rebecca B. Scott, B. Neyt, D. Brems Brems, K. Eekelers, A. J. Shortland y P. Degryse. "Experimental mixing of natron and plant ash style glass: implications for ancient glass recycling". Glass Technology: European Journal of Glass Science and Technology Part A 58, n.º 1 (14 de febrero de 2017): 8–16. http://dx.doi.org/10.13036/17533546.58.1.011.

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47

Elbanna, E., E. Amin, M. Ghazy y A. Badr. "The Reliance on some Groundwater Wells for Land Reclamation in Wadi El - Natron Region". Journal of Soil Sciences and Agricultural Engineering 9, n.º 2 (1 de febrero de 2018): 93–101. http://dx.doi.org/10.21608/jssae.2018.35580.

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Saidu, Yusuf, Maimuna Jumai Usman, Suleiman Ahmed Isa, Simeon Alabi Isezuo, Lawal Suleiman Bilbis, Saddiku Malam Sahabi, Ahmad Bello y Suleiman Alhaji Muhammad. "Biochemical and histological changes in the heart of post-partum rats exposed to Natron". Indian Heart Journal 70, n.º 6 (noviembre de 2018): 887–93. http://dx.doi.org/10.1016/j.ihj.2017.12.002.

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van den Bosch, Pim L. F., Marco de Graaff, Marc Fortuny-Picornell, Robin C. van Leerdam y Albert J. H. Janssen. "Inhibition of microbiological sulfide oxidation by methanethiol and dimethyl polysulfides at natron-alkaline conditions". Applied Microbiology and Biotechnology 83, n.º 3 (junio de 2009): 579–87. http://dx.doi.org/10.1007/s00253-009-1951-6.

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Diez-Martín, Fernando, Policarpo Sánchez Yustos, Diana Gómez de la Rúa, José Ángel Gómez González, Luis de Luque y Rebeca Barba. "Early Acheulean technology at Es2-Lepolosi (ancient MHS-Bayasi) in Peninj (Lake Natron, Tanzania)". Quaternary International 322-323 (febrero de 2014): 209–36. http://dx.doi.org/10.1016/j.quaint.2013.08.053.

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