CV Lattes
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Universidade Estadual de Campinas (UNICAMP). Instituto de Geociências (IG) (Institutional affiliation from the last research proposal) Birthplace: Brazil
Jacinta Enzweiler has a degree in Chemistry with an emphasis on Geochemistry from the Federal University of Rio Grande do Sul, a Master's degree in Chemistry, and a PhD in Science from the State University of Campinas-Unicamp. She did her post-doctorate in Analytical Geochemistry (1993-1994) at the Department of Earth Sciences, Open University, England. Full professor at Unicamp's Institute of Geosciences and a National Council for Scientific and Technological Development (CNPq) Research Productivity Fellow. In Geosciences, she dedicated her professional activities to Analytical Geochemistry, specifically to developing measurement methods for application in the chemical and isotopic characterization of geological materials, and more recently to Environmental Geochemistry by studying, for instance, the distribution of rare earth elements in surface and groundwater. Member of the Management Committees of the Isotope Geology and Geochemistry Laboratories, both at IG/Unicamp. She is co-editor-in-chief of the journal Geostandards and Geoanalytical Research (2016-present) and President (2018-2024) of the International Association of Geoanalysts (IAG). (Source: Lattes Curriculum)
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Between 2013 and 2017, periods of drought generated a water supply crisis that affected 48% of Brazilian municipalities, causing severe public health and economic problems at a national scale. Traditional solutions, based on centralized single-source water systems, have been ineffective in Brazil and developing countries. The main objective of this project is to create new hydro-economic …
In aquifers, the primary source of dissolved inorganic constituents in groundwater are water-rock reactions. The water composition reflects dissolution, precipitation, sorption, ion-exchange, and redox reactions that depend on the prevalent physicochemical and biotic conditions. The uranium concentration in natural waters tends to be low (< 1 µg/L) and values higher than 30 µg/L (provisio…
(Only some records are available in English at this moment)
The Araguaia Orogen represents part of the amalgamation history of the Gondwana Supercontinent during the late Neoproterozoic. The metasedimentary sequences record the tectonic history of the development and formation of this geotectonic unit. However, tectono-metamorphic studies performed in these sequences are rare and the existing works have a regional character. This scientific initia…
The appearance of the first complex organisms during the Ediacaran period (635 to 541 Ma) is one of the most notable episodes in Earth's history. Nevertheless, the causes that led to such life evolution remain still unclear. One of the hypotheses is the enhanced influx of nutrients into the ocean via chemical weathering of newly formed large continental masses. Such high nutrient availabi…
Natural waters contain trace elements as part of their dissolved constituents. Among them are the lanthanides (Ln) that with scandium and yttrium form the rare earth elements (REE). These elements find a wide range of technological uses and as a result they are being introduced in the environment, at levels never registered before. This research intends to characterize the occurrence of d…
he rise of the first complex organisms at the end of the Ediacaran period (635 to 541 Ma) is one of the most intriguing episodes in the history of the Planet. The causes for such move of life to its complex forms remain unclear. An enhanced influx of nutrients into the ocean via chemical weathering of large continental masses is one of the leading hypotheses to explain it. This high nutri…
| 1 / 1 | Ongoing grants |
| 16 / 7 | Completed research grants |
| 5 / 3 | Completed scholarships in Brazil |
| 2 / 1 | Completed scholarships abroad |
| 24 / 12 | All research grants and scholarships |
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