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Acidification processes in soils with different acid buffering capacity in Cryptomeria japonica and Chamaecyparis obtusa forests over two decades

机译:在过去的二十年里,日本柳杉和钝角沙棘林具有不同酸缓冲能力的土壤酸化过程

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Although plant soil interactions play important roles in regulating soil acidity, it remains unclear whether the species influence is changeable across soil acidity gradients. We resampled soils in eight stands of Ctyptomeria japonica and seven stands of Chamaecyparis obtusa in which soil chemical properties were documented in the 1990s. Half of the sites for each species had soils with a high acid buffering capacity (ABC), and the remaining sites had soils with a low ABC. ABC was defined by two criteria: the concentration of exchangeable base cations and the concentration of exchangeable Al. The aims of this study were (i) to characterize the accumulation of base cations and exchangeable Al by both tree species in high- or low-ABC soil profiles down to a depth of 40 cm and (ii) to clarify the changes of soil ABC in stands of C japonica or C obtusa grown in high- or low-ABC soil over the past two decades. In the low-ABC group, Ca depletion and Al accumulation were observed in both species. Potassium depletion also occurred in C obtusa stands. In contrast, high-ABC soils showed different trends. In C japonica soils, Ca accumulated during this period and sharp distinctions in exchangeable Ca concentrations were observed between the uppermost soil horizons and deeper horizons; however, in C. obtusa soils such distinctions were not evident and depletions both Ca and K occurred. These results suggest that plant soil interactions differed in the two soils. We speculate that C japonica accumulates Ca in soils with high ABC but loses this trait in low-ABC soils, meaning that C japonica responds to an acidic environment with a positive feedback of soil acid buffering capacity, such that ABC becomes greater in a high-ABC soil and smaller in a low-ABC soil. It appears that C obtusa promotes depletion of cations such as Ca and K and accumulation of exchangeable Al in soils regardless of ABC. Neither C japonica nor C obtusa is suitable for planting in nutrient-poor soils as they promote a shortage of base cations and an increase in Al toxicity. (C) 2014 Elsevier B.V. All rights reserved.
机译:尽管植物与土壤的相互作用在调节土壤酸度中起着重要作用,但尚不清楚物种的影响是否随土壤酸度梯度的变化而变化。我们重新采样了八种日本小草和七种Chamaecyparis obtusa的土壤,这些土壤在1990年代记录了土壤化学性质。每个物种一半的地点的土壤具有高酸缓冲能力(ABC),其余的地点的土壤具有低ABC。 ABC由两个标准定义:可交换的碱性阳离子的浓度和可交换的Al的浓度。这项研究的目的是(i)表征低至40 cm深度的高或低ABC土壤剖面中两种树种的碱性阳离子和可交换Al的积累,以及(ii)阐明土壤ABC的变化在过去的20年中,在高ABC或低ABC的土壤中种植的C. japonica或C. obtusa。在低ABC组中,两种物种均观察到Ca耗竭和Al积累。钝角果林还发生钾耗竭。相反,高ABC土壤表现出不同的趋势。在日本粳稻土壤中,Ca在此期间积累,并且在最上层土壤层和较深层土壤层之间观察到可交换的Ca浓度的明显差异。然而,在钝角梭菌土壤中,这种区别并不明显,并且钙和钾都发生了消耗。这些结果表明在两种土壤中植物土壤的相互作用是不同的。我们推测粳稻在ABC较高的土壤中会积累钙,但在低ABC的土壤中会失去此特性,这意味着粳稻对酸性环境的反应是对土壤酸缓冲能力的正反馈,因此在高土壤中ABC会变大。 ABC土壤,在低ABC土壤中较小。不论ABC如何,钝角C似乎促进了诸如Ca和K等阳离子的消耗以及土壤中可交换Al的积累。粳稻和钝柏都不适合在营养贫瘠的土壤中种植,因为它们会促进碱性阳离子的缺乏和铝毒性的增加。 (C)2014 Elsevier B.V.保留所有权利。

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