Analysis of the Throughfall Leachates of a Declining Forest in Relation to Time and to the Mineral Content of the Canopy

1992 ◽  
pp. 604-605
Author(s):  
D. Bouya ◽  
C. Myttenaere
Keyword(s):  
Mineral Content

Influence of anthropometric parameters on assessment of paediatric bone mineral density and bone mineral content

2013 ◽  
Author(s):  
N Hangartner Thomas ◽  
F Short David ◽  
Gilsanz Vicente ◽  
J Kalkwarf Heidi ◽  
M Lappe Joan ◽  
...  
Keyword(s):  
Bone Mineral Density ◽  
Bone Mineral Content ◽  
Bone Mineral ◽  
Mineral Content ◽  
Mineral Density ◽  
Anthropometric Parameters

Age at onset of walking affects bone mineral content in early childhood

2017 ◽  
Author(s):  
Saara Valkama ◽  
Heli Viljakainen ◽  
Elisa Holmlund-Suila ◽  
Jenni Rosendahl ◽  
Helena Hauta-alus ◽  
...  
Keyword(s):  
Early Childhood ◽  
Bone Mineral Content ◽  
Bone Mineral ◽  
Mineral Content ◽  
Age At Onset

Treatment with a TR[alpha]1 antagonist increases bone mineral content

2014 ◽  
Author(s):  
Julian A Waung ◽  
J H Duncan Bassett ◽  
Graham R Williams
Keyword(s):  
Bone Mineral Content ◽  
Bone Mineral ◽  
Mineral Content

Effects of preparation methods on the mineral content of tofu

2007 ◽  
Vol 17 (4) ◽  
pp. 342-347
Author(s):  
Satoko Tanaka ◽  
Toshiko Morisita ◽  
Kenji Chayama
Keyword(s):  
Mineral Content ◽  
Preparation Methods

Depositional Environment Drive as Overpressure Generation: Study Case in “Gap” Field, North West Java Basin

2020 ◽  
Author(s):  
A., C. Prasetyo
Keyword(s):  
Clay Mineral ◽  
Depositional Environment ◽  
Mineral Content ◽  
Hydrocarbon Generation ◽  
Well Test ◽  
Burial History ◽  
The South ◽  
North West ◽  
The North ◽  
Geological Processes

Overpressure existence represents a geological hazard; therefore, an accurate pore pressure prediction is critical for well planning and drilling procedures, etc. Overpressure is a geological phenomenon usually generated by two mechanisms, loading (disequilibrium compaction) and unloading mechanisms (diagenesis and hydrocarbon generation) and they are all geological processes. This research was conducted based on analytical and descriptive methods integrated with well data including wireline log, laboratory test and well test data. This research was conducted based on quantitative estimate of pore pressures using the Eaton Method. The stages are determining shale intervals with GR logs, calculating vertical stress/overburden stress values, determining normal compaction trends, making cross plots of sonic logs against density logs, calculating geothermal gradients, analyzing hydrocarbon maturity, and calculating sedimentation rates with burial history. The research conducted an analysis method on the distribution of clay mineral composition to determine depositional environment and its relationship to overpressure. The wells include GAP-01, GAP-02, GAP-03, and GAP-04 which has an overpressure zone range at depth 8501-10988 ft. The pressure value within the 4 wells has a range between 4358-7451 Psi. Overpressure mechanism in the GAP field is caused by non-loading mechanism (clay mineral diagenesis and hydrocarbon maturation). Overpressure distribution is controlled by its stratigraphy. Therefore, it is possible overpressure is spread quite broadly, especially in the low morphology of the “GAP” Field. This relates to the delta depositional environment with thick shale. Based on clay minerals distribution, the northern part (GAP 02 & 03) has more clay mineral content compared to the south and this can be interpreted increasingly towards sea (low energy regime) and facies turned into pro-delta. Overpressure might be found shallower in the north than the south due to higher clay mineral content present to the north.

Bone mineral content in the calcaneus after ankle fracture

1988 ◽  
Vol 59 (2) ◽  
pp. 173-175 ◽  
Author(s):  
Torbjorn Ahl ◽  
Hans-Erik Sjoberg ◽  
Nils Dalen
Keyword(s):  
Bone Mineral Content ◽  
Bone Mineral ◽  
Ankle Fracture ◽  
Mineral Content

Correlation Between Femur and Metatarsal Mineral Content in Swine

2011 ◽  
Author(s):  
Jillian Lekander ◽  
Kenneth J. Stalder ◽  
Anna K. Johnson ◽  
Tom Crenshaw ◽  
Locke A. Karriker
Keyword(s):  
Mineral Content
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