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首页> 外文期刊>Communications in Soil Science and Plant Analysis >Post-reclamation Age Effects on Soil Physical Properties and Microbial Activity Under Forest and Pasture Ecosystems
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Post-reclamation Age Effects on Soil Physical Properties and Microbial Activity Under Forest and Pasture Ecosystems

机译:林和牧场生态系统下土壤物理性质和微生物活性的后裂转年龄影响

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摘要

During surface mining and subsequent reclamation efforts, physical, chemical, and biological properties of soils are disturbed. A study was conducted to evaluate the effects of age chronosequence on soil physical property and microbial activity in chronosequence reclaimed sites covering successional ages in the ranges 1, 4, 8, 11, and 13 years under forest and pasture ecosystems. The adjacent normal and unmined pasture and forest were used as a control for comparison purposes. The study site was located at the Red Hill Mine in east central Mississippi (approximately 33.3 N latitude and 89 W longitude), which is used by the North America Mining Company, LLC. Soil samples were collected from the reclaimed and unmined sites at 0-15- and 15-30-cm depth and analyzed for selected soil quality indicators. Results indicated that water stable aggregate and infiltration were increased, but soil bulk density and compaction decreased with increasing reclamation age. Soil penetration resistance was greater in the pasture than forest ecosystem. All reclaimed soils had less microbial enzyme activity than an unmined forest ecosystem; however, bacteria population level after 11 years since reclamation was similar to that of unmined forest soils. Soil organic carbon increased with increasing reclamation age strongly correlated with soil physical indicators and appears to be the main driving force during the development of soil physical and biological properties in the humid southeast.
机译:在表面采矿过程中和随后的填海努力,物理,化学和土壤的生物学性质受到干扰。进行了一项研究,以评估年龄一致性对森林和牧草生生态系统下的1,4,8,11和13岁的成绩级恢复地点的成分后期地区土壤物理性质和微生物活性的影响。相邻的正常和未绕进的牧场和森林被用作比较目的的控制。该研究网站位于密西西比州东部的红山地区(大约33.3米纬度和89 W经度),由北美矿业公司LLC使用。从0-15-30cm的再生和未挤出的位点收集土壤样品,深入收集,并分析选定的土壤质量指标。结果表明,水稳定的聚集体和渗透率增加,但随着填海时期的增加,土壤堆积密度和压实减少。在牧场比森林生态系统的土壤渗透性较大。所有回收的土壤都具有比未切割的森林生态系统更少的微生物酶活性;然而,由于填海层的11年后细菌人口水平与未被灌注的森林土壤相似。土壤有机碳随着与土壤物理指标强烈相关的累积年龄的增加而增加,似乎是潮湿的东南地区土壤物理和生物学性质发展过程中的主要动力。

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