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首页> 外文期刊>Journal of Forest Science >Influence of a planting hole application of dolomitic limestone powder and basalt grit on the growth of Carpathian birch (Betula carpatica W. et K.) and soil chemistry in the air-polluted Jizerske hory Mts.
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Influence of a planting hole application of dolomitic limestone powder and basalt grit on the growth of Carpathian birch (Betula carpatica W. et K.) and soil chemistry in the air-polluted Jizerske hory Mts.

机译:在空气污染的Jizerske hory山中,施用白云质石灰石粉和玄武岩粗砂对生石灰的种植孔对喀尔巴阡桦树(Betula carpatica W. et K.)的生长和土壤化学的影响。

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摘要

The objective of the study was to evaluate the growth potential of Carpathian birch (Betula carpatica W. et K.) at an environmentally harsh mountain site and a response of this species to altered soil chemistry after dolomitic limestone and basalt grit applications. The Carpathian birch proved to be a suitable species for the replanting of extreme acidic mountain sites. This birch shows a low mortality rate, grows well in the clear-felled patches and soon forms a cover which is necessary for the reintroducing of more sensitive tree species. The application of dolomitic limestone and basalt grit resulted in the slower growth of Carpathian birch plantations. Liming raised soil reaction, sum of exchangeable bases, base saturation, cation exchange capacity and reduced exchangeable Al content. On the other hand, liming decreased an amount of oxidizable soil organic matter and negatively affected soil N, exchangeable P and K. Basalt grit increased exchangeable P and K contents and raised soil reaction, however only slightly. The influence of basalt grit on the sum of exchangeable bases, base saturation and cation exchange capacity was also less pronounced compared to liming. Basalt grit elevated the proportion of exchangeable aluminium and reduced the content of soil N.
机译:这项研究的目的是评估喀尔巴阡桦树(Betula carpatica W. et K.)在环境恶劣的山区的生长潜力,以及该物种对白云石石灰石和玄武岩砂砾施用后土壤化学变化的响应。喀尔巴阡桦树被证明是适合极端酸性山区重新种植的物种。该桦树显示出较低的死亡率,在开阔的小片中生长良好,并很快形成了覆盖物,这对于重新引入更敏感的树种是必需的。白云质石灰岩和玄武岩砂的应用导致喀尔巴阡桦树人工林的生长较慢。石灰提高了土壤反应,可交换碱的总和,碱饱和度,阳离子交换容量和减少的可交换Al含量。另一方面,石灰添加减少了可氧化的土壤有机质的数量,并对土壤中的氮,可交换的P和K产生了负面影响。玄武岩砂粒增加了可交换的P和K含量并提高了土壤反应,但仅增加了一点。与石灰相比,玄武岩砂对可交换碱之和,碱饱和度和阳离子交换容量的影响也不太明显。玄武岩砂提高了可交换铝的比例并减少了土壤N的含量。

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