scholarly journals Sediment Management of Reservoirs in Volcanic Area: Case of Wlingi and Lodoyo Reservoirs in Indonesia

Author(s):  
Fahmi Hidayat ◽  
Pitojo T. Juwono ◽  
Agus Suharyanto ◽  
Alwafi Pujiraharjo ◽  
Djoko Legono ◽  
...  
1979 ◽  
Author(s):  
M. Dean Kleinkopf ◽  
Donald L. Peterson ◽  
Robert E. Mattick
Keyword(s):  

2006 ◽  
Author(s):  
Bart Chadwick ◽  
Vikki Kirtay ◽  
Amy Blake ◽  
Ernie Arias ◽  
Bradley Davidson ◽  
...  

2006 ◽  
Author(s):  
D. B. Chadwick ◽  
Vikki Kirtay ◽  
Amy Blake ◽  
Ernie Arias ◽  
Bradley Davidson ◽  
...  

Author(s):  
Caterina Ledda ◽  
Claudia Lombardo ◽  
Elisabetta A. Tendi ◽  
Maria Hagnas ◽  
Gianluca Paravizzini ◽  
...  

: Fluoro-edenite (FE) is an asbestos-like amphibole present in the bentonitic lavas extracted from a stone quarry in Biancavilla, a village sited in the Etnean Volcanic Area (Italy). : Thoracic pathologies are the results of excessive inflammatory processes that are the early response of the immune system to inhaled fibers. As demonstrated for asbestos, fibers may trigger immune system cells in an acute and/or chronic manner. This review aims to clarify the pathways of inflammation in workers exposed to FE fibers. : Based on the articles reviewed, it seems that a permanent stimulus created by repeatedly inhaling the FE fibers and their persistence in the body can act as trigger both in promoting inflammatory processes and in immunological induction of autoimmune disease.


1994 ◽  
Vol 61 (3-4) ◽  
pp. 225-237 ◽  
Author(s):  
Alessandro Amato ◽  
Claudio Chiarabba ◽  
Massimo Cocco ◽  
Massimo di Bona ◽  
Giulio Selvaggi

Plants ◽  
2021 ◽  
Vol 10 (4) ◽  
pp. 673
Author(s):  
Fabián Augusto Aldaba Aldaba Núñez ◽  
Emily Veltjen ◽  
Esteban Manuel Martínez Martínez Salas ◽  
Marie-Stéphanie Samain

The Mexican state of Veracruz has suffered very high deforestation rates in the last few decades, and despite the establishment of protected areas and conservation projects, primary forest is now mainly persisting in mostly small, scattered, fragmented remnants. New species of Magnolia section Talauma in this state have been described with little to no reference to the already existing ones, potentially resulting in over-splitting, obscuring their taxonomic delineation and conservation status, and consequently conservation programs. To study the conservation units and their genetic diversity, we here employ 15 microsatellite markers on a highly representative sampling of 254 individuals of what are presumed to be five Magnolia species. The results support at least three species and maximum five main conservation units. We propose downgrading the latter to four, given morphological, ecological, demographical, and geographical considerations. Two out of the three sympatrically occurring species in the rainforest in the Los Tuxtlas volcanic area have weak genetic evidence to be considered separate species. Similarly, the individuals in the Sierra de Zongolica in central Veracruz, who bear a very high morphological and genetic similarity to Magnolia mexicana, have weak genetic evidence to be recognised as a separate species. Nonetheless, the individuals could be identified as Magnolia decastroi based on morphology, and further research including the full range of this species is recommended.


Minerals ◽  
2021 ◽  
Vol 11 (7) ◽  
pp. 721
Author(s):  
Ukhwan Byun ◽  
A.J. (Tom) van Loon ◽  
Kyoungtae Ko

The Gyeokpori Formation in the Buan volcanic area primarily contains siliciclastic rocks interbedded with volcanoclastics. These sediments are characterized by a variety of soft-sediment deformation structures (SSDS). The SSDS in the Gyeokpori Formation are embedded in poorly sorted conglomerates; slump folds are also present in the formation. The deformation mechanisms and triggers causing the deformation are not yet clear. In the present study, the trigger of the SSDS in the Gyeokpori Formation was investigated using facies analysis. This included evaluation of the reworking process of both cohesive and non-cohesive sediments. The analysis indicates that the SSDS are directly or indirectly associated with the alternation of conglomerates and mud layers with clasts. These layers underwent non-cohesive and cohesive deformation, respectively, which promoted SSDS formation. The slump folds were controlled by the extent of cohesive and non-cohesive deformation experienced by the sediment layers in the slope environment. The SSDS deformation style and morphology differ, particularly in the case of reworking by slump activity. This study contributes to the understanding of lacustrine slope-related soft-sediment deformation structures.


Author(s):  
Chien-Min Su ◽  
Wei-Jhe Wu ◽  
Strong Wen ◽  
Yi-Heng Li ◽  
Yen-Che Liao ◽  
...  

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