首页> 外文期刊>Arid Land Research and Management >Influence of topsoil depth on plant and soil attributes of 24-year old reclaimed mined lands.
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Influence of topsoil depth on plant and soil attributes of 24-year old reclaimed mined lands.

机译:表土深度对24岁复垦雷区植物和土壤属性的影响。

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摘要

Topsoil replacement on reclaimed mine lands is vital for improved infiltration, plant rooting media, enhanced nutrient cycling, and as a potential source of plant propagules to increase plant community diversity. Varying topsoil depth may influence reclamation success. This study assessed the long-term (24 years) effects of four topsoil replacement depths (0, 20, 40, and 60 cm) on plant community attributes (species richness, diversity, canopy cover, and production) and soil characteristics (viz., organic carbon (C), total nitrogen (N), available phosphorus (P), pH, soluble cations, electrical conductivity (EC), and cumulative water infiltration). The study site was established in the spring 1977 at Pathfinder Mining Corporation's Shirley Basin uranium mine in south-central Wyoming, USA. Artemisia tridentata ssp. wyomingensis, A. frigida, Pascopyrum smithii, Pseudoroegneria spicatum [Elymus spicatus], Stipa comata and Bouteloua gracilis comprise the dominant plant species on the landscape. Species richness and diversity were highest at the 0 cm topsoil depth and lowest at the 60 cm topsoil depth. Percent canopy cover of grasses was highest (25%) at 60 cm and lowest (15%) at 0 cm topsoil depth. Percent forb cover was highest (6%) at the 0 cm depth and lowest (2%) at 60 cm topsoil depth. Seeded species cover was highest (12%) at the 40 cm depth, but was not significantly different from the other depths. Aboveground biomass was similar between the 40 (727 kg ha-1) and 60 cm (787 kg ha-1) topsoil depths and higher than the 0 (512 kg ha-1) and 20 cm (506 kg ha-1) replacement depths. Plant species richness and diversity decreased with increasing topsoil depth, while biomass increased. Organic C mass in the soil profile (75 cm) was greatest in the 60 cm topsoil replacement (18.7 t C ha-1) and lowest in the 0 and 20 cm treatments (11.3 and 10.5 t C ha-1, respectively). N mass (75 cm profile) exhibited a similar pattern with 60 cm of topsoil having the highest (1.9 t N ha-1) and the 0 and 20 cm the lowest (0.8 t N ha-1 and 0.9 t N ha-1, respectively). Cumulative water infiltration was highest (134 mm) for the 40 cm topsoil depth followed by 60 cm (116 mm), and lowest (61 mm) for the 0 cm treatment. Soil N, organic C, and infiltration data indicate topsoil replacement depths of 40 and 60 cm provide the best nutrient status and water storage potential for sustainable reclamation. Placement of shallow topsoil replacement depths should be carefully planned to ensure topsoil thickness is adequate to sustain a vegetative community capable of protecting the soil surface against erosion. Variable topsoil replacement depths can be used in reclamation to manipulate plant community characteristics and create a mosaic of vegetation types. However, the reduced vegetation cover observed at the shallower topsoil depths may not protect against soil erosion; therefore, using variable topsoil depth replacement as a reclamation practice will require careful planning and implementation..
机译:在开垦的矿山土地上替代表土对于改善渗透力,植物生根培养基,增强养分循环以及作为增加植物群落多样性的植物繁殖体的潜在来源至关重要。不同的表土深度可能会影响填海的成功。这项研究评估了四种表土替换深度(0、20、40和60 cm)对植物群落属性(物种丰富度,多样性,冠层覆盖度和产量)和土壤特征(即土壤)的长期(24年)影响。 ,有机碳(C),总氮(N),有效磷(P),pH,可溶性阳离子,电导率(EC)和累积水渗透)。该研究站点于1977年春季在美国怀俄明州中南部的Pathfinder Mining Corporation的Shirley Basin铀矿中建立。蒿(Artemisia tridentata ssp。)怀俄明州,福建曲霉,史密斯氏Pascopyrum smithii,假单胞菌(Pseudoroegneria spicatum [Elymus spicatus]),Stipa comata和Bouteloua gracilis是景观中的优势植物。物种丰富度和多样性在表土深度为0 cm时最高,而在表土深度为60 cm时最低。在60 cm的表土深度处,草冠层的百分数最高(25%),而在0 cm的深度最低(15%)。在0 cm深度,表层土壤覆盖率最高(6%),在60 cm表土深度处,覆盖率最低(2%)。种子物种的覆盖率在40厘米深度处最高(12%),但与其他深度没有显着差异。在40(727 kg ha-1)和60 cm(787 kg ha-1)的表土深度之间,地上生物量相似,并且高于0(512 kg ha-1)和20 cm(506 kg ha-1)的替代深度。 。随着表土深度的增加,植物物种的丰富度和多样性降低,而生物量增加。土壤剖面中的有机碳质量(75 cm)在60 cm的表土替代物中最大(18.7 t C ha-1),在0 cm和20 cm处理中最低(分别为11.3 t和10.5 t C ha-1)。 N质量(75 cm剖面)表现出相似的模式,其中60 cm的表土最高(1.9 t N ha-1),而0和20 cm的最低表土(0.8 t N ha-1和0.9 t N ha-1),分别)。对于40 cm的表土深度,累积水渗透最高(134 mm),其后为60 cm(116 mm),对于0 cm的处理,最低水渗透(61 mm)。土壤氮,有机碳和入渗数据表明表土置换深度为40和60厘米,可提供最佳养分状况和蓄水潜力,以实现可持续的垦殖。应仔细规划浅表土置换深度的布置,以确保表土厚度足以维持能够保护土壤表面免受侵蚀的植物群落。可变的表土置换深度可用于开垦中,以操纵植物群落特征并创建植被类型的镶嵌图。然而,在较浅的表层土壤深度观察到的植被减少可能无法防止土壤侵蚀。因此,使用可变的表土深度替代作为填海措施将需要仔细的计划和实施。

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