In search of novel water soluble forskolin analogues for positive inotropic activity

Using the novel lead from hydroxy acetyl substituted forskolin analogues, such as 7 beta-hydroxyacetyl-7 beta-deacetyl forskolin or 6 beta-hydroxyacetyl forskolin, a number of water soluble omega-amino acyl derivatives were synthesized. Two such compounds 6 and 18 showed better in vitro activity but failed to show in vivo activity.     

Mechanism of light fading of dyes on cellophane and poly(ethylene terephthalate)

Studies of relative rates of fading of dyes and Hammett σ-value of substituents in their molecules lead to further evidence that fading of azo dyes on Cellophane and poly-(ethylene terephthalate) is probably an oxidation type of reaction. Absorption spectra of the same dye on these two substrates tend to indicate a very high state of aggregation of dyes on Cellophane as compared to that on poly(ethylene terephthalate).     

SELF-DIFFUSION IN POTENTIALS OF MEAN FORCE IN WEAKLY- AND STRONGLY-INTERACTING DISPERSIONS

Studies of interactions in dispersions have traditionally focused on the stability and transport properties of such systems at extreme dilution, that is, at concentrations for which colloidal and hydrodynamic interactions are significant between at most two particles at a given time. In practice, however, dispersions of interest often do not satisfy this restriction, and, consequently, many-body colloidal interactions and hydrodynamic coupling have important roles in the observed macroscopic behavior. This paper presents an analysis of the effects of many-body interactions on the self-diffusion coefficient in interacting dispersions. Self-diffusion coefficients have been determined for dilute-gas dispersions and for Yukawa dispersions interacting through appropriate potentials of mean force. It is shown that the diffusion coefficients change negligibly with attraction for typical magnitudes of the Hamaker constant in an otherwise repulsion-dominated (i.e., stable) dispersion. The results show that, for thin electrical double layers, dilute dispersions can be approximated by hard-sphere dispersions, even for large values of surface potentials. However, for thick double layers (i.e., thickness comparable to particle radius), while the short-time diffusion coefficient is affected only negligibly, the long-time coefficient can decrease considerably because of the 'memory' effects—even for moderate or low values of the surface potentials. Corresponding results are presented for both dilute-gas dispersions and dispersions with significant local structures. The long-time diffusion coefficients in the latter are effectively linear in volume fraction (up to about 0.2)for thin double layers and are given with reasonable accuracy by the dilute-gas approximation.     

Cost of transmission transactions: an introduction

Major technical issues are discussed related to the cost of transmission transactions provided by a vertically integrated electric utility company. The authors identify the components of the cost of a transmission transaction and present methodologies for evaluating them using simple examples. The major cost components of a transmission transaction are: operating cost; opportunity cost; reinforcement cost; and existing system cost. The evaluation of these components requires the development of new analytical and knowledge-based techniques     

In vitro synthesis of molybdopterin from precursor Z using purified converting factor. Role of protein-bound sulfur in formation of the dithiolene

The pterin component of the molybdenum cofactor, termed molybdopterin, is synthesized in Escherichia coli by enzymes encoded at the chl loci. A late step in the biosynthetic pathway, the conversion of a molybdopterin intermediate, precursor Z, to molybdopterin, requires the activity of a two-subunit protein, the converting factor. Precursor Z has many of the features of molybdopterin but lacks the dithiolene function essential for molybdenum ligation. Conversion of precursor Z to molybdopterin is accomplished by transfer of sulfur to produce the dithiolene. The present study describes an in vitro system for molybdopterin biosynthesis comprised of purified precursor Z and purified converting factor. It is established that these components are sufficient to yield molybdopterin, identified by conversion to its characteristic products, Form A, Form B, and dicarboxamidomethylmolybdopterin. Under conditions of precursor excess, the formation of molybdopterin was stoichiometric with converting factor, as would be expected in the absence of a sulfur-regenerating system. The labile product of the reaction, molybdopterin, remained associated with the converting factor large subunit. These results establish that the source of sulfur for molybdopterin biosynthesis is the converting factor and suggest that in vivo a novel sulfur cycle must function to resupply sulfur to the converting factor.     

Formation of ethanol from carbon monoxide via a new microbial catalyst

A recently discovered clostridial bacteria converts components of synthesis gas (CO, CO₂, H₂) into liquid products such as ethanol, butanol and acetic acid. Isolated from an agricultural lagoon, the stability and productivity characteristics of the bacteria were studied in a continuous 4.5 l bubble column bioreactor at 37°C using artificial blends of CO, CO₂, and N₂. Preliminary results on the rates of cell growth, substrate utilization, product formation, and yields of products and cells from CO are discussed. At steady state, apparent yields (mole C in products per mole CO consumed) of ethanol, butanol, and acetic acid were 0.15, 0.075 and 0.025, respectively, and the cell yield was 0.25 g/mol CO. The theoretical yield of ethanol is 0.33 if CO is only utilized for the production of ethanol. The experimental yield of CO₂ from CO was approximately 60% compared to the theoretical yield of 67% with ethanol as the sole product. As a comparison with another ethanol-producing bacteria, the results of a similar fermentation study using batch-grown Clostridium ljungdahlii showed yields of 0.062 for ethanol and 0.094 for acetic acid and a cell yield of 1.378 g/mol.     

A multicenter community study on the efficacy of double-fortified salt

BACKGROUND: Iron and iodine deficiencies affect more than 30% of the world's population. Typical Indian diets contain adequate amounts of iron, but the bioavailability is poor. This serious limiting factor is caused by low intake of meat products rich in heme iron and intake of phytates in staple foods in the Indian diet, which inhibits iron absorption. OBJECTIVE: To test the stability of double-fortified salt (DFS) during storage and to assess its efficacy in improving the iron and iodine status of the communities. METHODS: The stability of both iodized salt and DFS during storage for a 2-year period was determined. The bioefficacy of DFS was assessed in communities covering three states of the country for a period of 1 year. This was a multicenter, single-blind trial covering seven clusters. The experimental group used DFS and the control group used iodized salt. The salts were used in all meals prepared for family members, but determination of hemoglobin by the cyanmethemoglobin method was performed in only two or three members per family, and not in children under 10 years of age (n = 393 and 436 in the experimental and control groups, respectively). The family size was usually four or five, with a male: female ratio of 1:1, consisting of two parents with two or three children. Hemoglobin was measured at baseline, 6 months (midpoint), and 12 months (endpoint). Urinary iodine was measured in only one cluster at baseline and endpoint. All the participants were dewormed at baseline, 6 months, and 12 months. RESULTS: The iron and iodine in the DFS were stable during storage for 2 years. Over a period of 1 year, there was an increase of 1.98 g/dL of hemoglobin in the experimental group and 0.77 g/dL of hemoglobin in the control group; the latter increase may have been due to deworming. The median urinary iodine changed from 200 microg/dL at baseline to 205 microg/dL at the end of the study in the experimental group and from 225 microg/dL to 220 microg/dL in the control group. There was a statistically significant (p < .05) improvement in the median urinary iodine status of subjects who were iodine deficient (urinary iodine < 100 microg/L) in both the experimental and the control groups, a result showing that DFS was as efficient as iodized salt in increasing urinary iodine from a deficient to sufficient status. There was a statistically significant increase (p < .05) in hemoglobin in all seven clusters in the experimental group compared with the control. CONCLUSIONS: The iron and iodine in the DFS are stable in storage for 2 years. The DFS has proved beneficial in the delivery of bioavailable iron and iodine.     

The origin of naturally occurring perchlorate: the role of atmospheric processes

Perchlorate, an iodide uptake inhibitor, is increasingly being detected in new places and new matrices. Perchlorate contamination has been attributed largelyto the manufacture and use of ammonium perchlorate (the oxidizer in solid fuel rockets) and/or the earlier use of Chilean nitrate as fertilizer (approximately 0.1% perchlorate). However, there are regions such as the southern high plains (Texas Panhandle) where there is no clear historical or current evidence of the extensive presence of rocket fuel or Chilean fertilizer sources. The occurrence of easily measurable concentrations of perchlorate in such places is difficult to understand. In the southern high plains groundwater, perchlorate is better correlated with iodate, known to be of atmospheric origin, compared to any other species. We show that perchlorate is readily formed by a variety of simulated atmospheric processes. For example, it is formed from chloride aerosol by electrical discharge and by exposing aqueous chloride to high concentrations of ozone. We report that perchlorate is present in many rain and snow samples. This strongly suggests that some perchlorate is formed in the atmosphere and a natural perchlorate background of atmospheric origin should exist.