在西弗吉尼亚州的一个露天煤矿,树木生长在撕裂、压实和轻微压实的灰色砂岩表土替代品上

L. Wilson-Kokes, J. Skousen
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引用次数: 0

摘要

陡峭的地形和稀薄的原生土壤是西维吉尼亚州南部采煤地区的特征。州和联邦法规要求在复垦期间更换原生表土以重建植被。由于在开采前收集这种薄层土壤的危险和费用,监管机构允许矿山经营者使用替代表土材料,包括风化(棕色)和未风化(灰色)的地质材料作为生长介质。对于牧场和海地开采后的土地利用,替代材料通过施肥和石灰化为牧草的建立和生长提供适宜的物理和化学性质。当重新造林是采矿后的土地利用时,西弗吉尼亚州的法规要求1.2米的天然表土和棕色风化砂岩层,但如果天然表土数量不足,可以使用未风化的材料。这项研究检查了在西弗吉尼亚州样品矿地表使用棕色和灰色砂岩材料作为生长介质的区域的树木生长情况。在该网站已经发表的一项研究中,我们发现棕色和灰色砂岩地块的树木生长有显著差异。在这项研究中,我们选择了两个额外的灰色砂岩地块与原始的棕色和灰色地块进行比较。两个原址为棕色砂岩压实和灰色砂岩压实,我们在附近增加了灰色砂岩轻度压实和灰色砂岩压实后撕裂的地块。灰色图的平均pH值在7.3到7.9之间,而棕色图的平均pH值为5.4。棕色砂岩上的树木生长是所有灰色砂岩样地树木生长的三倍以上。棕色密实样地的平均树木体积指数为3108 cm³,而灰色密实样地(909 cm³)、灰色轻度密实样地(407 cm³)和灰色破洞样地(885 cm³)的平均树木体积指数显著低于棕色密实样地(3108 cm³)。填海8年后,灰色砂岩地块,无论是轻微压实、压实还是撕裂,与棕色砂岩地块相比,树木生长都较差。灰色砂岩已被证明是该地点重新造林的次等表土替代品。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
TREE GROWTH ON RIPPED, COMPACTED, AND SLIGHTLY COMPACTED GRAY SANDSTONE TOPSOIL SUBSTITUTE ON A SURFACE COAL MINE IN WEST VIRGINIA 1
Steep topography and thin native soils characterize the coal mining regions of southern West Virginia. State and federal regulations require replacement of native topsoil during reclamation for re-establishment of a vegetative cover. Due to hazards and expense associated with collecting this thin layer of soil before mining, regulators have allowed mine operators to use substitute topsoil materials, including weathered (brown) and unweathered (gray) geologic materials for growth media. For pasture and hayland post-mining land uses, substitute materials provide suitable physical and chemical properties for establishment and growth of forages with fertilization and liming. When reforestation is the post-mining land use, regulations in West Virginia require a 1.2 m layer of native topsoil and brown weathered sandstone, but unweathered materials may be used if native topsoil quantities are insufficient. This study examined tree growth on areas where brown and gray sandstone materials were applied to the surface as growth media at the Samples Mine in West Virginia. In a study already published at this site, we found significant differences in tree growth on brown and gray sandstone plots. For this study, we selected two additional gray sandstone plots for comparison to the original brown and gray plots. The two original sites were brown sandstone compacted and gray sandstone compacted, and we added nearby plots of gray sandstone slightly compacted and gray sandstone compacted and then ripped. Average pH ranged from 7.3 to 7.9 on the gray plots compared to 5.4 on the brown plot. Tree growth on brown sandstone was more than triple that of tree growth on all of the gray sandstone plots. Mean tree volume index on the brown compacted plot was 3108 cm 3 while mean tree volume index was significantly lower on the gray compacted plot (909 cm³), the gray slightly compacted plot (407 cm 3 ), and the gray ripped plot (885 cm³). Eight years after reclamation, the gray sandstone plots, whether slightly compacted, compacted, or ripped, showed poor tree growth compared to brown sandstone. Gray sandstone has proven to be an inferior topsoil substitute for reforestation on this site.
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