On the mechanical effects of poroelastic crystal mush in classical magma chamber models

Author Posting. © American Geophysical Union, 2018. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Solid Earth 123(11), (2018): 9376-9406. doi: 10.1029/2018JB015985.Improved constraints on the mechanical behavior of magma chambers is essential for understanding volcanic processes; however, the role of crystal mush on the mechanical evolution of magma chambers has not yet been systematically studied. Existing magma chamber models typically consider magma chambers to be isolated melt bodies surrounded by elastic crust. In this study, we develop a physical model to account for the presence and properties of crystal mush in magma chambers and investigate its impact on the mechanical processes during and after injection of new magma. Our model assumes the magma chamber to be a spherical body consisting of a liquid core of fluid magma within a shell of crystal mush that behaves primarily as a poroelastic material. We investigate the characteristics of time‐dependent evolution in the magma chamber, both during and after the injection, and find that quantities such as overpressure and tensile stress continue to evolve after the injection has stopped, a feature that is absent in elastic (mushless) models. The time scales relevant to the postinjection evolution vary from hours to thousands of years, depending on the micromechanical properties of the mush, the viscosity of magma, and chamber size. We compare our poroelastic results to the behavior of a magma chamber with an effectively viscoelastic shell and find that only the poroelastic model displays a time scale dependence on the size of the chamber for any fixed mush volume fraction. This study demonstrates that crystal mush can significantly influence the mechanical behaviors of crustal magmatic reservoirs.We thank James Rice, Tushar Mittal, Chris Huber and Helge Gonnerman for useful discussions in the early stages of this work. S. Adam Soule was supported by National Science Foundation Grant OCE‐1333492. Meghan Jones was supported by the U.S. Department of Defense through the National Defense Science and Engineering Graduate Fellowship (NDSEG) Program. The numerical codes used for computing the results in the work can be found at https://github.com/YangVol/MushyChamber.2019-03-3

Submarine Lava Deltas of the 2018 Eruption of Kīlauea Volcano

Hawaiian and other ocean island lava flows that reach the coastline can deposit significant volumes of lava in submarine deltas. The catastrophic collapse of these deltas represents one of the most significant, but least predictable, volcanic hazards at ocean islands. The volume of lava deposited below sea level in delta-forming eruptions and the mechanisms of delta construction and destruction are rarely documented. Here, we report on bathymetric surveys and ROV observations following the Kīlauea 2018 eruption that, along with a comparison to the deltas formed at Pu‘u ‘Ō‘ō over the past decade, provide new insight into delta formation. Bathymetric differencing reveals that the 2018 deltas contain more than half of the total volume of lava erupted. In addition, we find that the 2018 deltas are comprised largely of coarse-grained volcanic breccias and intact lava flows, which contrast with those at Pu‘u ‘Ō‘ō that contain a large fraction of fine-grained hyaloclastite. We attribute this difference to less efficient fragmentation of the 2018 ‘a‘ā flows leading to fragmentation by collapse rather than hydrovolcanic explosion. We suggest a mechanistic model where the characteristic grain size influences the form and stability of the delta with fine grain size deltas (Pu‘u ‘Ō‘ō) experiencing larger landslides with greater run-out supported by increased pore pressure and with coarse grain size deltas (Kīlauea 2018) experiencing smaller landslides that quickly stop as the pore pressure rapidly dissipates. This difference, if validated for other lava deltas, would provide a means to assess potential delta stability in future eruptions

Overt hypoadrenalism is uncommon in patients with stage 3 and 4 bronchogenic carcinoma

Introduction. Lung cancer is the leading cause of cancer mortality in most countries. The adrenal glands are common sites of metastatic lung cancer as approximately 40% of subjects with stage 4 bronchogenic carcinoma have adrenal metastases. The prevalence of biochemical hypoadrenalism is, however, remarkably poorly documented.Objectives. Our study aimed to determine the prevalence of primary hypoadrenalism, as defined by a subnormal cortisol response to the 250 µg adrenocorticotrophic hormone (ACTH) stimulation test, in patients with stage 3 and 4 lung cancer.Methods. Thirty patients with stage 3 and 4 bronchogenic carcinoma were prospectively recruited from the bronchus clinic. Demographic data and electrolytes were recorded and each patient had a 250 µg ACTH stimulation test to determine the prevalence of overt adrenal insufficiency, defined as a +30 minute cortisol of less than 550 nmol/l.Results. The median age and quartile deviation was 62 (10) years and the median basal cortisol was 429.5 (321) nmol/l. The median peak cortisol was 828.5 (342) nmol/l (range 536 - 1 675 nmol/l). Twenty-eight patients (93.3%) had an appropriate rise of cortisol to greater than 550 nmol/l following 250 µg ACTH stimulation. Two patients (6.7%) had mild primary adrenal failure with a peak cortisol between 500 and 550 nmol/l associated with a raised plasma ACTH concentration (131.4 and 10.5 pmol/l, normal 2.2 - 10 pmol/l). Twenty-eight patients (92.9%) were normonatraemic, while the two hyponatraemic patients had biochemical evidence of the syndrome of inappropriate antidiuretic hormone secretion.Conclusion. In conclusion, despite evidence that the adrenal glands of patients with disseminated bronchogenic carcinoma are frequently affected by metastatic disease, biochemical evidence of clinically significant hypoadrenalism is relatively uncommon and is not accurately predicted by electrolyte abnormalities

The mechanical response of a magma chamber with poroviscoelastic crystal mush

Author Posting. © American Geophysical Union, 2021. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Solid Earth 126(4), (2021): e2020JB019395, https://doi.org/10.1029/2020JB019395.Improved understanding of the impact of crystal mush rheology on the response of magma chambers to magmatic events is critical for better understanding crustal igneous systems with abundant crystals. In this study, we extend an earlier model by Liao et al. (2018); https://doi.org/10.1029/2018jb015985 which considers the mechanical response of a magma chamber with poroelastic crystal mush, by including poroviscoelastic rheology of crystal mush. We find that the coexistence of the two mechanisms of poroelastic diffusion and viscoelastic relaxation causes the magma chamber to react to a magma injection event with more complex time-dependent behaviors. Specifically, we find that the system’s short-term evolution is dominated by the poroelastic diffusion process, while its long-term evolution is dominated by the viscoelastic relaxation process. We identify two post-injection timescales that represent these two stages and examine their relation to the material properties of the system. We find that better constraints on the poroelastic diffusion time are more important for the potential interpretation of surface deformation using the model

Contribution of growth hormone-releasing hormone and somatostatin to decreased growth hormone secretion in elderly men

Objective. The pathophysiology of the decline in circulating growth hormone (GH) concentrations that may occur with ageing remains elusive. We have investigated the potential contributions of decreased endogenous GH-releasing hormone (GHRH) and increased somatostatin secretion to this phenomenon.Design and methods. The strategy used was to stimulate GH secretion in 8 young (20 - 24 years old, body mass index (BMI) 22.8 ± 2.8 kg/m2) and 8 elderly (68- 82 years old, BMI 23.4 ± 1.6 kg/m2) male subjects on separate occasions by means of: (i) intravenous bolus 0.5 ).lg/kg D-Ala2 GHRH(1-29)-NH alone; (ii) 0.5 μg/kg GHRH after pretreatment with two oral doses of 50 mg atenolol (to inhibit somatostatin secretion); (iii) 1.25 mg oral bromocriptine alone (to increase endogenous GHRH and/or inhibit somatostatin); (iv) 50 mg oral atenolol plus 1.25 mg oral bromocriptine; and (v) 0.5 μg/kg GHRH after pre-treatment with 1.25 mg oral bromocriptine.Results. The elderly men had a significantly lower peak and area under curve (AUC) GH response to intravenous GHRH when compared with 8 young men (peak 3.1 ± 1.0 ng/ml v. 21.6 ± 5.0 ng/ ml, AUC 205 ±56 ng/ ml/min v.1 315 ± 295 ng/ ml/ min, P < 0.05). Pre-treatment with atenolol before GHRH administration produced no significant increase in peak and AUC GH response in both groups, whlch remained lower in the elderly men than in their young counterparts (peak 5.5 ±1.8 ng/ ml v. 29.3 ± 7.0 ng/ml, AUC 327 ± 90 ng/ml/min v. 2 017 ± 590 ng/ ml/min, P < 0.05). Bromocriptine alone did not cause a significant rise in GH concentration in either elderly or young subjects (peak 3.1 ± 1.1 v. 8.8 ± 3.2 ng/ ml, P > 0.05). When atenolol was administered before bromocriptine, both groups responded but the elderly subjects had a significantly greater peak and AUC response (peak 3.6 ± 0.7 v. 10:7 ± 2.1 ng/ ml; AUC 191 ± 39 v. 533 ± 125 ng/ ml/ min, P < 0.05). Bromocriptine given before GHRH failed to potentiate GHRH action on GH release in either group. Of 5 elderly men who tmderwent further evaluation of GH secretory ability, 2 subjects had GH levels > 10 ng/ rnl, either basally or after intravenous GHRH. The remaining 3 had an initially impaired GH response to bolus intravenous GHRH. After 100 μg GHRH subcutaneously twice daily for up to 2 weeks the GH responses to intravenous bolus GHRH (0.5μg /kg) were reassessed. One exhibited a normal response (> 10 ng/ rnl) after 1 week of daily GHRH treatment, another had a nearnormal response after 2 weeks (9.7 ng/ rnl), while the third still had an impaired response by the end of the 2-week treatment period (3.2 ng/ ml).Conclusions. The restoration of endogenous GH secretion in these elderly subjects by means of GHRH priming, and the failure of manipulation of somatostatinergic tone to restore a normal GH response to GHRH suggests that somatotroph atrophy due to a reduction in endogenous GHRH secretion is the principal cause of the diminished GH secretion with ageing

Identification of Erosional Terraces on Seamounts: Implications for Interisland Connectivity and Subsidence in the Galápagos Archipelago

Shallow seamounts at ocean island hotspots and in other settings may record emergence histories in the form of submarine erosional terraces. Exposure histories are valuable for constraining paleo-elevations and sea levels in the absence of more traditional markers, such as drowned coral reefs. However, similar features can also be produced through primary volcanic processes, which complicate the use of terraced seamounts as an indicator of paleo-shorelines. In the western Galápagos Archipelago, we utilize newly collected bathymetry along with seafloor observations from human-occupied submersibles to document the location and depth of erosional terraces on seamounts near the islands of Santiago, Santa Cruz, Floreana, Isabela, and Fernandina. We directly observed erosional features on 22 seamounts with terraces. We use these observations and bathymetric analysis to develop a framework to identify terrace-like morphologic features and classify them as either erosional or volcanic in origin. From this framework we identify 79 erosional terraces on 30 seamounts that are presently found at depths of 30 to 300 m. Although intermittent subaerial connectivity between the islands has been hypothesized, the depths of these erosional terraces in the Santiago region are the first direct evidence of paleo-connectivity in the modern archipelago. Collectively, the terraces have non-randomly distributed depths. We suggest that peaks in the distribution of terrace depths likely represent long durations of exposure (i.e., sea-level still or lowstands). By comparing these peaks to those of subsidence adjusted sea-level curves, we identify the average subsidence rate that best reproduces the observed terrace distributions. These rates are 0.2–0.4 m/ka for this portion of the central Galápagos, since the formation of the seamounts, consistent with previous independent estimates. Using these subsidence rates and evidence for erosional terraces at depths up to 300 m, we conclude that all islands in the central archipelago have been intermittently connected starting between 435 and 900 ka. Individual island pairs have likely been repeatedly subaerially connected for short intervals since that time

Navigational infrastructure at the East Pacific Rise 9°50′N area following the 2005–2006 eruption : seafloor benchmarks and near-bottom multibeam surveys

Author Posting. © American Geophysical Union, 2008. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geochemistry Geophysics Geosystems 9 (2008):Q11T04, doi:10.1029/2008GC002070.Four seafloor benchmarks were deployed with ROV Jason2 at frequently visited areas along the northern East Pacific Rise (NEPR) ridge crest near 9°50′N, within the Ridge2000 EPR integrated study site (ISS) bull's eye. When used in concert with established deep-ocean acoustic positioning techniques, these benchmarks provide navigational infrastructure to facilitate the integration of near-bottom data at this site by allowing efficient and quantitative coregistration of data and observations collected on multiple dives and over multiple cruises. High-resolution, near-bottom multibeam bathymetric surveys also were conducted along and across the ridge crest to provide a morphological and geological context for the benchmark areas. We describe the navigation and data processing techniques used to constrain the benchmark positions and outline operational details to effectively use benchmarks at this and other deep-ocean sites where multidisciplinary time series studies are conducted. The well-constrained positions of the benchmarks provide a consistent geospatial framework that can be used to limit navigational uncertainties during seafloor sampling and mapping programs and enable accurate spatial coregistration and integration of observations. These data are important to test a range of multidisciplinary hypotheses that seek to link geological, chemical, and biological processes associated with crustal accretion and energy transfer from the mantle to the hydrosphere at mid-ocean ridges

Performances laitiere et economique des vaches metisses (gir x borgou) complementees avec la dreche de sorgho au paturage a panicum maximum C1 dans le nord-Benin

Dans les pays en développement, la demande en lait et produits laitiers ne cesse de croître. Pour cela, une expérimentation a été menée à la Ferme d’Elevage d’Okpara (FEO) au Bénin pour évaluer l’effet de la complémentation à base de la drêche de sorgho sur les performances laitières et économiques des vaches allaitantes (Gir x Borgou). Cette étude a porté sur 21 femelles âgées de 6,33 ± 0,57 ans dont le numéro de lactation est égal à 2,33 ± 0,57. Ces animaux ont été répartis en trois lots homogènes (lot 1 ; lot 2 et lot 3) de 7 animaux chacun, recevant respectivement 0, 1 et 2 kg de complément. L’aliment de base de ces animaux était le Panicum maximum var. C1 du pâturage. Les performances laitières étaient suivies pendant 98 jours. Après l’analyse de variance (ANOVA) à un effet sur le logiciel Minitab 17, les valeurs moyennes ont été comparées par le test de Tukey. En moyenne, le lot 1 a produit 1,14 ± 0,44 kg de lait par jour (kg lait/jour) ; le lot 2, 2,03 ± 0,54 kg lait/jour et le lot 3, 3,00 ± 0,41 kg lait/jour. Ces données sont significativement différentes (P<0,05) d’un lot à un autre. Les efficacités alimentaires ont été respectivement de 2,11 ± 0,03 et 1,61 ± 0,02 chez les lots complémentés. En investissant 100 F CFA dans la complémentation avec la drêche de sorgho, l’éleveur gagne 190 F CFA et 406 F CFA respectivement au niveau des lots 2 et 3. L’utilisation de la drêche de sorgho dans l’alimentation des vaches métisses pour la production de lait est donc très bénéfique. Mots clés : Vaches métisses, pâturage, drêche de sorgho, performances, Nord-Bénin.  English Title:  Dairy and economic performance of mixed cows (gir x borgou) complemented with sorgho brewer’s on <i>Panicum maximum</i> C1 grazing in Northen Benin In developing countries, the demand for milk and dairy products continues to grow. For this, an experiment was carried out at the Okpara Farm (FEO) in Benin to assess the effect of complementation with dry sorghum brewer’s on the milk and economic  performance of suckler cows (Gir x Borgou ). This study involved 21 females aged 6.33 ± 0.57 years whose lactation number was 2.33 ± 0.57. These animals were divided into three homogeneous lots (lot 1; lot 2 and lot 3) of 7 animals each, receiving 0, 1 and 2 kg of supplement respectively. The staple food of these animals was Panicum maximum var. C1 of the pasture. Milk performance was monitored for 98 days. After an effect analysis of variance (ANOVA) on Minitab 17 software, the mean values were compared by the Tukey test. On average, lot 1 produced 1.14 ± 0.44 kg of milk per day (kg milk / day); lot 2, 2.03 ± 0.54 kg milk / day and lot 3, 3.00 ± 0.41 kg milk / day. These data are significantly different (P<0.05) from one batch to another. Food efficiencies were 2.11 ± 0.03 and 1.61 ± 0.02, respectively, in the complemented lots. By investing 100 FCFA in the complementation with sorghum brewer’s, the farmer earns 190 FCFA and 406 FCFA respectively in lots 2 and 3. The use of sorghum brewer’s in the feeding of mixed-breed cows for the production of milk is therefore very beneficial. Key words: Mixed cows, pasture, sorghum brewer’s, performances, North-Benin