نتایج جستجو برای: deep water

تعداد نتایج: 745168  

2015
Sigrid Skoglund Anna Siwertsson Per-Arne Amundsen Rune Knudsen

Morphological divergence was evident among three sympatric morphs of Arctic charr (Salvelinus alpinus (L.)) that are ecologically diverged along the shallow-, deep-water resource axis in a subarctic postglacial lake (Norway). The two deep-water (profundal) spawning morphs, a benthivore (PB-morph) and a piscivore (PP-morph), have evolved under identical abiotic conditions with constant low light...

Journal: :مجله علوم کشاورزی ایران 0
علیرضا سلطانی قلعه جوقی محمد لغوی

field capacity, fuel consumption and drive wheel slippage in massey ferguson (mf399) tractor with standard and liquid ballasted (630 kg) axle load and at 4wd mode was evaluated and compared. the tests were conducted at the experimental station, college of agriculture, shiraz university, in a field with clay loam soil at average moisture content of 18% d.b. the experiment was of a randomized com...

2014
Valentina Magni Pierre Bouilhol Jeroen van Hunen

We investigate the dehydration processes in subduction zones and their implications for the water cycle throughout Earth's history. We use a numerical tool that combines thermo-mechanical models with a thermodynamic database to examine slab dehydration for present-day and early Earth settings and its consequences for the deep water recycling. We investigate the reactions responsible for releasi...

Journal: :Science 2007
J C Duplessy D M Roche M Kageyama

Oxygen isotope analysis of benthic foraminifera in deep sea cores from the Atlantic and Southern Oceans shows that during the last interglacial period, North Atlantic Deep Water (NADW) was 0.4 degrees +/- 0.2 degrees C warmer than today, whereas Antarctic Bottom Water temperatures were unchanged. Model simulations show that this distribution of deep water temperatures can be explained as a resp...

ژورنال: ژئومکانیک نفت 2019

There have been many studies on reservoir compaction where different mechanisms being suggested as the reasons behind the integrity of unconsolidated reservoirs during production. Theory of poroelasticity is often used to evaluate the likelihood of compaction under these circumstances, but it is often failed to explain the creep behavior of unconsolidated formations. In this study, attempts are...

Journal: :Nature communications 2015
Rosina Grimm Ernst Maier-Reimer Uwe Mikolajewicz Gerhard Schmiedl Katharina Müller-Navarra Fanny Adloff Katharine M Grant Martin Ziegler Lucas J Lourens Kay-Christian Emeis

Recurrent deposition of organic-rich sediment layers (sapropels) in the eastern Mediterranean Sea is caused by complex interactions between climatic and biogeochemical processes. Disentangling these influences is therefore important for Mediterranean palaeo-studies in particular, and for understanding ocean feedback processes in general. Crucially, sapropels are diagnostic of anoxic deep-water ...

Journal: :پژوهش های جغرافیایی (منتشر نمی‏شود) 0
سید حسن مطیعی لنگرودی استاد دانشکده جغرافیا - دانشگاه تهران سعد ا... ولایتی دانشیار گروه جغرافیا - دانشگاه فردوسی مشهد فرحناز اکبر اقلی دانشجوی دوره دکتری برنامه ریزی روستایی، دانشگاه فردوسی مشهد

abstract from 165 millions cubic meters of water which is used in kalat region, 60 millions cubic meters is surface water and 105 millions cubic meters is underground water. most of water needed in this region, is provided by the rivers. there is not any problem for providing water in agricultural section, drinking water and hygiene sections in the region. the most important problem in the regi...

2005
M.-L. TIMMERMANS P. WINSOR J. A. WHITEHEAD

The Arctic Ocean likely impacts global climate through its effect on the rate of deep-water formation and the subsequent influence on global thermohaline circulation. Here, the renewal of the deep waters in the isolated Canadian Basin is quanitified. Using hydraulic theory and hydrographic observations, the authors calculate the magnitude of this renewal where circumstances have thus far preven...

Journal: :Monthly Weather Review 1924

Journal: :Proceedings of the London Mathematical Society 1905

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