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首页> 外文期刊>Journal of plant nutrition and soil science >The coarse-soil fraction is the main living space of fungal hyphae in the BhBs horizon of a Podzol
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The coarse-soil fraction is the main living space of fungal hyphae in the BhBs horizon of a Podzol

机译:粗土部分是Podzol BhBs层中真菌菌丝的主要生存空间

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In acidified forest soils, the coarse-soil fraction is a potential nutrient source. Plant nutrient uptake from the coarse-soil fraction is aided by ectomycorrhiza. Similarly, (recalcitrant) organic matter (OM) is an important nutrient source largely made plant-available through (symbiotic) microorganisms, especially in the topsoil. We hypothesized that in a podzol profile, fungal hyphae would concentrate in nutrient hotspots, either OM or the coarse-soil fraction. Absolute hyphal length, base saturation, and organic-C content of a Podzol profile were determined in the fine-earth and coarse-soil fractions. In the fine-earth fraction, hyphae were attracted by the organic-C content and relative high base saturation. In the coarse-soil fraction of the BhBs horizon, the absolute hyphal length exceeded the hyphal length in the fine earth by factor 3, yet C content and base saturation were lowest. We could not determine to what fungi the hyphae belonged. Most likely ectomycorrhiza, ericoid mycorrhiza and saprotrophic fungi dominate the upper soil layers of this profile and all utilize OM for nutrition. In the deeper mineral horizons and especially in the coarse-soil fraction, ectomycorrhiza are better adapted than other fungi to harvest nutrients from inorganic sources. Additionally, favorable physical properties may explain the high amount of fungal hyphae in the coarse-soil fraction of the BhBs horizon. Both the coarse-soil fraction and deeper mineral soil horizons may play a more active role in microbial nutrient cycling than previously assumed.
机译:在酸化的森林土壤中,粗土部分是潜在的养分来源。外生菌根有助于从粗土中吸收植物养分。同样,(顽固性)有机物(OM)是一种重要的营养来源,很大程度上是通过(共生)微生物特别是在表土中通过植物获得的。我们假设在Podzol谱中,真菌菌丝会集中在营养热点,无论是OM还是粗土部分。在细土和粗土中确定了绝对菌丝长度,碱基饱和度和Podzol轮廓中的有机碳含量。在细土部分中,菌丝被有机碳含量和相对较高的碱饱和度吸引。在BhBs层的粗土部分中,绝对菌丝长度超过细土中的菌丝长度3倍,而C含量和碱饱和度最低。我们无法确定菌丝属于哪种真菌。最有可能的是外生菌根,类固醇菌根和腐生真菌在该剖面的上层土壤中占主导地位,并且都利用OM进行营养。在更深的矿物层中,特别是在粗土部分,根除菌根比其他真菌更适合从无机资源中获取营养。此外,良好的物理特性可以解释BhBs层中粗土部分中大量的真菌菌丝。与以前的假设相比,粗土含量和更深的矿质土壤视野都可能在微生物养分循环中发挥更积极的作用。

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