首页> 外文期刊>Soil Biology & Biochemistry >Response of soil C and N transformations to tannin fractions originating from Scots pine and Norway spruce needles.
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Response of soil C and N transformations to tannin fractions originating from Scots pine and Norway spruce needles.

机译:土壤碳和氮转化对源自苏格兰松树和挪威云杉针的单宁含量的响应。

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Tannins are polyphenolic compounds that may influence litter decomposition, humus formation, nutrient (especially N) cycling and ultimately, plant nutrition and growth. The aim of this study was to determine the response of C and N transformations in soil to tannins of different molecular weight from Norway spruce (Picea abies (L.) Karst) and Scots pine (Pinus sylvestris L.) needles, tannic acid and cellulose. Arginine was added to test whether the soil microbial community was limited by the amount of N, and arginine+tannin treatments were used to test whether the effects of tannins could be counteracted by adding N. Soil and needle samples were taken from adjacent 70-year-old Scots pine and Norway spruce stands located in Kivalo, northern Finland. Tannins were extracted from needles and fractioned based on molecular weight; the fractions were then characterized by LC-MS and GC-MS. Light fractions contained tannin monomers and dimers as well as many other compounds, whereas heavy fractions consisted predominantly of polymerized condensed tannins. Spruce needles contained more procyanidin than prodelphinidin units, while in pine needles prodelphinidin units seemed to be dominant. The fractions were added to soil samples, pine fractions to pine soil and spruce fractions to spruce soil, and incubated at 14 degrees C for 6 weeks. CO2 evolution was followed throughout the experiment, and the rates of net mineralization of N and net nitrification, concentration of dissolved organic N (DON) and amounts of microbial biomass C and N were measured at the end of the experiment. The main effects of the fractions were similar in both soils. Light fractions strongly enhanced respiration and decreased net N mineralization, indicating higher immobilization of N in the microbial biomass. On the contrary, heavy fractions reduced respiration and slightly increased net N mineralization, suggesting toxic or protein-precipitating effects. The effects of tannic acid and cellulose resembled those of light fractions. DON concentrations generally decreased during incubation and were lower with heavy fractions than with light fractions. No clear differences were detected between the effects of light and heavy fractions on microbial biomass C and N. Treatments that included addition of arginine generally showed trends similar to treatments without it, although some differences between light and heavy fractions became more obvious with arginine than without it. Overall, light fractions seemed to act as a labile source of C for microbes, while heavy fractions were inhibitors..
机译:单宁是多酚化合物,可能影响凋落物分解,腐殖质形成,养分(尤其是氮)循环,并最终影响植物的营养和生长。这项研究的目的是确定土壤中碳和氮的转化对来自挪威云杉(Picea abies(L.)Karst)和苏格兰松树(Pinus sylvestris L.)针,鞣酸和纤维素的不同分子量单宁的响应。添加精氨酸以测试土壤微生物群落是否受到氮含量的限制,精氨酸+单宁处理用于测试是否可以通过添加氮来抵消单宁的影响。土壤和针头样品取自相邻的70年古老的苏格兰松树和挪威云杉林位于芬兰北部的基瓦洛。从针头中提取单宁,并根据分子量进行分馏;然后通过LC-MS和GC-MS表征级分。轻质馏分包含单宁单体和二聚体以及许多其他化合物,而重质馏分主要由聚合的缩合单宁组成。云杉针头中原花青素的含量高于原花青素单位,而在松针中原花青素的单位似乎占主导。将这些级分添加到土壤样品中,将杉木级分添加到松土中,将云杉级分添加到云杉土中,并在14摄氏度下孵育6周。在整个实验过程中都跟踪二氧化碳的排放,并在实验结束时测量了氮的净矿化率和净硝化率,溶解的有机氮(DON)浓度以及微生物量碳和氮的含量。在两种土壤中,馏分的主要作用相似。轻组分强烈地增强了呼吸作用并减少了净氮矿化,表明微生物生物量中氮的固定化更高。相反,大量的碎片减少了呼吸作用,净氮净矿化略有增加,表明具有毒性或蛋白质沉淀作用。单宁酸和纤维素的作用类似于轻质馏分。 DON的浓度通常在孵育过程中降低,重馏分的浓度低于轻馏分的浓度。在轻质和重质馏分对微生物生物量碳和氮的影响之间未发现明显差异。包括添加精氨酸的处理通常显示出与不使用精氨酸的处理相似的趋势,尽管精氨酸和重质馏分之间的一些差异比不使用精氨酸时更为明显。它。总体而言,轻馏分似乎是微生物的不稳定C来源,而重馏分是抑制剂。

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