During acute oral intoxication by cadmium compounds, gastrointestinal epithelial damage contributes to immediate toxicity. However, secondary systemic toxicity may develop due to intestinal uptake of cadmium. This review presents an evaluation of the effects of chelators on the acute toxicity of cadmium after parenteral or oral exposure and on the intestinal uptake of cadmium. This review shows:
Chelating agents may affect the acute toxicity of cadmium in a variety of ways depending on the exposure route for cadmium and administration route for the chelator.
With regard to survival, systemic toxicity of absorbed cadmium is of major importance, as intraperitoneal administration of chelators could eliminate or reduce mortality due to orally administered cadmium chloride.
Lipophilicity of chelators and their cadmium complexes may result in extensively augmented intestinal uptake. However, hydrophilic chelators may efficiently reduce the intestinal cadmium uptake.
For hydrophilic chelators, the stability of the cadmium complex is an important determining factor of efficacy.
The optimal oral antidote towards orally administered cadmium are the BAL analogs, especially DMSA, while the optimal intraperitoneal antidotes towards orally or intraperitoneally administered cadmium are the higher members of the polyaminopolycarboxylate family, especially TTHA.
When administered simultaneously (DMSA orally and TTHA intraperitoneally), these chelators synergistically reduce the whole‐body retention of cadmium.
In conclusion, chelation treatment in acute oral cadmium intoxication should first prevent/reduce intestinal damage and uptake by rapid oral administration of a chelating antidote and then alleviate systemic toxicity due to absorbed cadmium and enhance renal/biliary cadmium excretion by parenteral administration of a chelating antidote. 相似文献
Cations in soil are essential for the growth of plants and micro-organisms. Their availability is dependent on soil organic matter. Soil organic matter (SOM) is heterogeneous comprising amino, aliphatic and phenolic acids, but particularly humic substances. All these substances can complex cations selectively. Mechanisms of complexation with dissolved organic matter are discussed. Such complexation can lead to the apparently contradictory observations that dissolved organic matter (DOM) can either increase the concentration of some less soluble nutrients, making them more available for plant uptake, or make them less available and hence less toxic. the importance of DOM is discussed in relation to soil solution, particularly the rhizosphere, and also in relation to aquatic systems. the latter systems contain mainly dissolved humic substances whereas in the soil, non-humic substances assume a greater importance.
SOM in the rhizosphere is derived from plant, microbial and animal remains but much, especially the water-soluble compounds, are acquired through root exudation. Exudation has important consequences for enhanced nutrient availability as a result of the production of non-humic substances such as amino, aliphatic and phenolic acids. in future, the role of root exudation in relation to DOM and nutrient availability should be investigated more fully, particularly as predicted elevated CO2 levels are likely to have a major impact on root exudation, nutrient availability, and possibly ecosystem community structure and functioning. It is likely that more information will become available on aquatic systems as more highly sensitive techniques and equipment capable of dealing with low concentrations of DOM in these systems become available. 相似文献