Pearson John, Stewart George R
Department of Biology (Darwin), University College London, Gower Street, London, WCIE 6BT, UK.
Department of Botany, University of Queensland, Brisbane, Qld 4072, Australia.
New Phytol. 1993 Oct;125(2):283-305. doi: 10.1111/j.1469-8137.1993.tb03882.x.
Across Europe, total nitrogen deposition is increasing and, of this total, atmospheric ammonia can contribute up to 50-80%. Average deposition of ammonia in the UK is likely to be around 15-20 kg ha yr , while in The Netherlands, which has some of the highest rates of deposition, this value is likely to be between 40 and 50 kg ha yr . It is argued that because of the processes of assimilation and nitrification this ammonia is an acidifying pollutant. Ammonia taken up by plants is most likely to be directly assimilated and this uptake can have a strong effect on the nutrient imbalances of the plant. With root uptake in particular, anions are taken up in preference to cations. However, simple soil/plant nutrient measurements are unlikely to be a definitive means of monitoring ammonia pollution. This is because the processes of ammonia metabolism and acidification affect soil ion activity, mycorrhizas, plant uptake, and foliar leaching. These effects interact with acidity per se, and are compounded by the strong correlative co-deposition of ammonia with sulphur. Evidence for uptake of gaseous and wet deposited ammonia by leaves is presented. The exact mechanism of ammonia toxicity is still not really clear, but could be due to physiological perturbation, rather than to the direct toxicity of the ion. Assimilation of ammonia by leaves releases protons which can cause cellular acidosis, and has important implications for acid-base regulation in cells. This regulation depends on intrinsic features of the plant's metabolism, that is in turn dependent on the ecology of root versus leaf nitrogen nutrition under normal conditions. Certain species are more acidic in a leaf physiological sense and tend to be prone to damage by pollutants. Likewise, acidic habitats are particularly prone to damage through both eutrophication and the different capacities of plants both to utilize and to buffer against this nitrogen enrichment. The current evidence from The Netherlands suggests that the part this plays in perturbing the ecosystem should not be underestimated. Contents Summary 283 I. Introduction 284 II. Emission and deposition of ammonia 284 III. Is ammonia toxic? 288 IV. The eflfects of ammonia deposition 289 V. Throughfall versus foliar uptake 293 VI. Physiological effects on ahove-ground parts 296 VII. Conclusions 301 Acknowledgements 302 References 302.
在整个欧洲,总氮沉降量正在增加,其中大气氨的贡献率可达50%-80%。英国氨的平均沉降量可能约为每年每公顷15-20千克,而在沉积率较高的荷兰,这一数值可能在每年每公顷40至50千克之间。有人认为,由于同化和硝化作用,这种氨是一种酸化污染物。植物吸收的氨最有可能被直接同化,这种吸收会对植物的养分失衡产生强烈影响。特别是通过根系吸收时,阴离子优先于阳离子被吸收。然而,简单的土壤/植物养分测量不太可能成为监测氨污染的决定性手段。这是因为氨代谢和酸化过程会影响土壤离子活性、菌根、植物吸收和叶片淋溶。这些影响与酸度本身相互作用,并因氨与硫的强烈相关共沉积而加剧。文中给出了叶片吸收气态和湿沉降氨的证据。氨毒性的确切机制仍不太清楚,但可能是由于生理扰动,而非离子的直接毒性。叶片对氨的同化会释放质子,从而导致细胞酸中毒,这对细胞内的酸碱调节具有重要意义。这种调节取决于植物新陈代谢的内在特征,而这又反过来取决于正常条件下根系与叶片氮营养的生态情况。某些物种在叶片生理意义上更易酸化,往往更容易受到污染物的损害。同样,酸性生境特别容易因富营养化以及植物利用和缓冲这种氮富集的不同能力而受到损害。来自荷兰的现有证据表明,这在扰乱生态系统中所起的作用不应被低估。内容摘要283 一、引言284 二、氨的排放与沉降284 三、氨有毒吗?288 四、氨沉降的影响289 五、穿透雨与叶片吸收293 六、对地上部分的生理影响296 七、结论301 致谢302 参考文献302