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At least 865 records · Page 48Linked to original sources
PubMed2002

Humic acid induces apoptosis in human endothelial cells.

Humic acid (HA) has been implicated as an etiologic factor in the vasculopathy of Blackfoot disease. In this study, the ability of HA to induce apoptosis was studied in cultured human umbilical vein endothelial cells. Treatment of endothelial cells with a variety of concentrations of HA (50-200 microg/ml) resulted in dose- and time-dependent sequences of events marked by apoptosis as shown by loss of cell viability, chromatin condensation, and internucleosomal DNA fragmentation. Antioxidants (superoxide dismutase, vitamin C, and vitamin E) and Ca(2+) chelator (BAPTA) effectively suppressed HA-induced DNA fragmentation (apoptosis). Further studies have shown that HA induced dramatic Ca(2+)-dependent caspase activation (2, 3, 6, 8, and 9). In contrast, negligible caspase-1 activation was observed. The increase in HA-induced apoptosis correlated with a reduction in Bcl-2, a potent cell death inhibitor, and an increase in Bax protein levels, which heterodimerizes with and thereby inhibits Bcl-2. Both of the antioxidants vitamin C and vitamin E prevented the dysregulation of Bcl-2 and Bax in HA-treated endothelial cells. Furthermore, the increase in p53 protein levels correlated with an increase in HA-induced apoptosis. We concluded that both Ca(2+) and oxidative stress were mediators of apoptosis caused by HA and the induction of apoptotic cell death on endothelial cells may be important to the etiology of HA-induced vascular disorder of Blackfoot disease.

Apoptosis↗
PubMed1995

Enhanced biodegradation of aromatic pollutants in cocultures of anaerobic and aerobic bacterial consortia.

Toxic aromatic pollutants, concentrated in industrial wastes and contaminated sites, can potentially be eliminated by low cost bioremediation systems. Most commonly, the goal of these treatment systems is directed at providing optimum environmental conditions for the mineralization of the pollutants by naturally occurring microflora. Electrophilic aromatic pollutants with multiple chloro, nitro and azo groups have proven to be persistent to biodegradation by aerobic bacteria. These compounds are readily reduced by anaerobic consortia to lower chlorinated aromatics or aromatic amines but are not mineralized further. The reduction increases the susceptibility of the aromatic molecule for oxygenolytic attack. Sequencing anaerobic and and aerobic biotreatment steps provide enhanced mineralization of many electrophilic aromatic pollutants. The combined activity of anaerobic and aerobic bacteria can also be obtained in a single treatment step if the bacteria are immobilized in particulate matrices (e.g. biofilm, soil aggregate, etc.). Due to the rapid uptake of oxygen by aerobes and facultative bacteria compared to the slow diffusion of oxygen, oxygen penetration into active biofilms seldom exceeds several hundred micrometers. The anaerobic microniches established inside the biofilms can be applied to the reduction of electron withdrawing functional groups in order to prepare recalcitrant aromatic compounds for further mineralization in the aerobic outer layer of the biofilm. Aside from mineralization, polyhydroxylated and chlorinated phenols as well as nitroaromatics and aromatic amines are susceptible to polymerization in aerobic environments. Consequently an alternative approach for bioremediation systems can be directed towards incorporating these aromatic pollutants into detoxified humic-like substances. The activation of aromatic pollutants for polymerization can potentially be encouraged by an anaerobic pretreatment step prior to oxidation. Anaerobic bacteria can modify aromatic pollutants by demethylating methoxy groups and reducing nitro groups. The resulting phenols and aromatic amines are readily polymerized in a subsequent aerobic step.

Bacteria, Aerobic↗
PubMed1994

The growth of fractal humic acids: cluster correlation and gel formation.

The growth of humic acids, prepared by a gentle method from two different kinds of soils (I and II), has been studied using small-angle neutron scattering at an acidity corresponding to pH 5.0 and 0.10 M ionic strength (NaCl). Humic acids aggregate either to large clusters with a fractal dimension of 2.3 and an average diameter of 1720 A (I) or to clusters with an average diameter of 700 A (II). After storage for 2 days at 4 degrees C, the latter aggregates (II) formed a gel. In a step toward gelation, we observed cluster-cluster interaction from the neutron-scattering data in the form of a correlation peak. These differences in size can be explained by assuming that the smaller particles (II) are trapped into a nonequilibrium state characterized by the temperature-solvent condition. The importance of a humic acid gel network for the conservation of water and nutrients in the environment is discussed.

Gels↗