环境中的锂及其对高等植物的影响

R. Kastori, I. Maksimović, Marina Putnikdelić
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引用次数: 1

摘要

锂(Li)以低浓度存在于生物圈的所有部分,包括生物体内。它主要通过母基质在成土过程中受到的自然过程以及由于人为活动而到达陆地环境。不同土壤类型的锂含量不同;例如,盐渍土和壤土的锂含量较高。它主要以离子形式存在于地表水和地下水的水环境中,浓度很低。它在土壤中是可移动的,因此土壤被Li污染会导致其在地下水中的浓度升高。在环境中,锂从锂排放源到达大气。它被广泛应用于许多行业,最近在电子产品的锂离子电池中,由于它可能对环境造成潜在的风险。陆生植物主要通过土壤中的根吸收锂,但也通过大气中的芽吸收锂。在土壤中,锂主要与粘土组分和有机质结合。在植物的吸收、运输和分配过程中,它表现得像碱土离子,而不是碱离子。Li在韧皮部不动的事实支持了这一说法。其上升输送主要取决于蒸腾强度。植物从酸性土壤中吸收的锂比从碱性土壤中吸收的多。Li对植物的生长发育并不是必需的。在低浓度下,它可以刺激和影响植物的化学成分和有机生产。Li在盐生植物的代谢中起着重要的作用。它越来越被认为是动物和人类必需的微量元素,并被用于治疗痴呆症、自杀意念、攻击和暴力的人类药物中。高浓度的锂对所有植物都是有毒的,但对锂的吸收和敏感性取决于物种。毛茛科、茄科和菊科的一些代表性植物的Li积累量增加,而禾科、百合科、芸苔科、樱叶科的Li积累量较低。高浓度的Li对植物的许多生理生化过程(DNA、RNA和蛋白质途径、水分关系、光合色素含量、光合作用、活性氧产生、细胞膜脂质过氧化等)产生不利影响,进一步表现为生长发育迟缓、发育障碍、视觉症状、叶脉间坏死和叶缘坏死。超积累植物提取大量的锂,因此用于植物修复。更好地了解Li的有益浓度和植物毒性浓度对植物代谢和生长发育的影响,对于提高对高等植物Li生物活性的认识至关重要。
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Lithium in the Environment and its Effects on Higher Plants
Summary Lithium (Li) is present in low concentrations in all parts of the biosphere, including living organisms. It reaches the terrestrial environment primarily through natural processes to which parent substrate was subjected during pedogenesis, and due to anthropogenic activities. Individual soil types differ regarding Li content; for example saline and loamy soils have higher Li content. It is found in low concentrations primarily in ionic form in aquatic environments in surface and groundwater. It is mobile in the soil and thus soil contamination with Li can lead to its higher concentration in groundwater. In the environment, Li reaches the atmosphere from Li-emitting sources. It is widely used in many industries, lately in the Li-ion batteries in electronic goods, due to which it may be a potential risk for the environment. Terrestrial plants take up Li largely via roots from the soil, but also via shoots from the atmosphere. In the soil, Li is mostly bound by clay fraction and organic matter. During the uptake, transport and distribution in plants it behaves like an alkaline earth ion, not like an alkali ion. The fact that Li is immobile in the phloem supports this claim. Its ascendent transport mainly depends upon the transpiration intensity. More Li is taken up by plants from acid soils than from alkaline soils. Li is non-essential for plant growth and development. In low concentrations it can be stimulative and affect chemical composition and organic production of plants. Li plays an important role in the metabolism of halophyte species. It is increasingly regarded as an essential trace element for animals and humans, and used in human medication to treat dementia, suicidal ideation, aggression and violence. High levels of Li are toxic to all plants, but uptake and sensitivity to Li are species-dependent. Some representatives of the Ranunculaceae, Solanaceae and Asteraceae families are characterized by increased Li accumulation, while Poaceae, Liliaceae, Brassicaceae, Caprifoliaceae show low accumulation. High concentrations of Li have adverse effects on many physiological and biochemical processes in plants (DNA, RNA and protein pathways, water relations, content of photosynthetic pigments, photosynthesis, production of reactive oxygen species, lipid peroxidation of the cell membranes etc.), which is further manifested as stunted growth, developmental disorder, visual symptoms, interveinal necrosis and necrosis along the leaf margins. Hyperaccumulator plants extract significant amounts of Li and are therefore used in phytoremediation. Better understanding of the effects of beneficial and phytotoxic concentrations of Li on metabolism and plant growth and development remains vital for the improvement of the knowledge about biological activity of Li in higher plants.
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