Brine rejection leads to salt-fingers in seasonally ice-covered lakes

When ice forms on the surface of lakes, dissolved salts are pushed out of the ice into the liquid water below. If enough salt is rejected from the ice, the excess weight of the salt can lead to long `fingers` of salty fluid moving from the ice into the water below. We ran a series of experiments to investigate these `fingers' and conclude that this process occurs in most freshwater lakes that freeze annually. This process is important for the evolution of lakes, and how they will be different as fewer lakes freeze

Measurement of stimulated Hawking emission in an analogue system

There is a mathematical analogy between the propagation of fields in a general relativistic space-time and long (shallow water) surface waves on moving water. Hawking argued that black holes emit thermal radiation via a quantum spontaneous emission. Similar arguments predict the same effect near wave horizons in fluid flow. By placing a streamlined obstacle into an open channel flow we create a region of high velocity over the obstacle that can include wave horizons. Long waves propagating upstream towards this region are blocked and converted into short (deep water) waves. This is the analogue of the stimulated emission by a white hole (the time inverse of a black hole), and our measurements of the amplitudes of the converted waves demonstrate the thermal nature of the conversion process for this system. Given the close relationship between stimulated and spontaneous emission, our findings attest to the generality of the Hawking process.Comment: 7 pages, 5 figures. This version corrects a processing error in the final graph 5b which multiplied the vertical axis by 2. The graph, and the data used from it, have been corrected. Some minor typos have also been corrected. This version also uses TeX rather than Wor

Scanning mutagenesis of the I-II loop of the Cav2.2 calcium channel identifies residues Arginine 376 and Valine 416 as molecular determinants of voltage dependent G protein inhibition

Direct interaction with the β subunit of the heterotrimeric G protein complex causes voltage-dependent inhibition of N-type calcium channels. To further characterize the molecular determinants of this interaction, we performed scanning mutagenesis of residues 372-387 and 410-428 of the N-type channel α1 subunit, in which individual residues were replaced by either alanine or cysteine. We coexpressed wild type Gβ1γ2 subunits with either wild type or point mutant N-type calcium channels, and voltage-dependent, G protein-mediated inhibition of the channels (VDI) was assessed using patch clamp recordings. The resulting data indicate that Arg376 and Val416 of the α1 subunit, residues which are surface-exposed in the presence of the calcium channel β subunit, contribute significantly to the functional inhibition by Gβ1. To further characterize the roles of Arg376 and Val416 in this interaction, we performed secondary mutagenesis of these residues, coexpressing the resulting mutants with wild type Gβ1γ2 subunits and with several isoforms of the auxiliary β subunit of the N-type channel, again assessing VDI using patch clamp recordings. The results confirm the importance of Arg376 for G protein-mediated inhibition and show that a single amino acid substitution to phenylalanine drastically alters the abilities of auxiliary calcium channel subunits to regulate G protein inhibition of the channel

MP745: A Long-Term Study of an Oak Pine Forest Ecosystem: A Brief Overview of the Holt Research Forest

This publication provides an overview of the long-term forest ecosystem project at the Holt Research Forest in Arrowsic, Maine. It is based on nearly 16 years of work by an interdisciplinary team from the College of Natural Sciences, Forestry, and Agriculture, including faculty, professional staff, visiting scientists, University of Maine graduate students, and undergraduate field assistants. We hope this publication will be useful to other researchers, to our workshop participants, and to others interested in forest ecosystem science.https://digitalcommons.library.umaine.edu/aes_miscpubs/1029/thumbnail.jp

Instability in stratified shear flow: Review of a physical interpretation based on interacting waves

Instability in homogeneous and density stratified shear flows may be interpreted in terms of the interaction of two (or more) otherwise free waves in the velocity and density profiles. These waves exist on gradients of vorticity and density, and instability results when two fundamental conditions are satisfied: (I) the phase speeds of the waves are stationary with respect to each other ("phase-locking"), and (II) the relative phase of the waves is such that a mutual growth occurs. The advantage of the wave interaction approach is that it provides a physical interpretation to shear flow instability. This paper is largely intended to purvey the basics of this physical interpretation to the reader, while both reviewing and consolidating previous work on the topic. The interpretation is shown to provide a framework for understanding many classical and nonintuitive results from the stability of stratified shear flows, such as the Rayleigh and Fjørtoft theorems, and the destabilizing effect of an otherwise stable density stratification. Finally, we describe an application of the theory to a geophysical-scale flow in the Fraser River estuary

Scanning mutagenesis of omega-atracotoxin-Hv1a reveals a spatially restricted epitope that confers selective activity against insect calcium channels

We constructed a complete panel of alanine mutants of the insect-specific calcium channel blocker omega-atracotoxin-Hv1a. Lethality assays using these mutant toxins identified three spatially contiguous residues, Pro(10), Asn(27), and Arg(35), that are critical for insecticidal activity against flies (Musca domestica) and crickets (Acheta domestica). Competitive binding assays using radiolabeled omega-atracotoxin-Hv1a and neuronal membranes prepared from the heads of American cockroaches (Periplaneta americana) confirmed the importance of these three residues for binding of the toxin to target calcium channels presumably expressed in the insect membranes. At concentrations up to 10 muM, omega-atracotoxin-Hv1a had no effect on heterologously expressed rat Ca(v)2.1, Ca(v)2.2, and Ca(v)1.2 calcium channels, consistent with the previously reported insect selectivity of the toxin. 30 muM omega-atracotoxin-Hv1a inhibited rat Ca-v currents by 10-34%, depending on the channel subtype, and this low level of inhibition was essentially unchanged when Asn(27) and Arg(35), which appears to be critical for interaction of the toxin with insect Ca-v channels, were both mutated to alanine. We propose that the spatially contiguous epitope formed by Pro(10), Asn(27), and Arg(35) confers specific binding to insect Ca-v channels and is largely responsible for the remarkable phyletic selectivity of omega-atracotoxin-Hv1a. This epitope provides a structural template for rational design of chemical insecticides that selectively target insect Ca-v channels