首页> 外文期刊>European Journal of Soil Science >Microbial CO production, CH dynamics and nitrogen in a wetland soil (New York State, USA) associated with three plant species (Typha, Lythrum, Phalaris)
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Microbial CO production, CH dynamics and nitrogen in a wetland soil (New York State, USA) associated with three plant species (Typha, Lythrum, Phalaris)

机译:与三种植物物种(香蒲,千屈菜,plant菜)相关的湿地土壤(美国纽约州)中的微生物CO生成,CH动态和氮

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Plants furnish soil with organic carbon (OC) compounds that fuel soil microorganisms, but whether individual plant species - or plants with unique traits - do so uniquely is uncertain. We evaluated soil microbial processes within a wetland in which areas dominated by a distinct plant species (cattail -Typha sp.; purple loosestrife -Lythrum salicaria L.; reed canarygrass -Phalaris arundinacea L.) co-mingled. We also established an experimental plot with plant shoot removal. The Phalaris area had more acidic soil pH (7.08 vs. 7.27-7.57), greater amount of soil organic matter (19.0% vs. 9.0-11.5%), and the slowest production rates of CO (0.10 vs. 0.21-0.46 omol kgp# sp#) and CH (0.040 vs. 0.054-0.079 nmol kgp# sp#). Nitrogen cycling was dominated by net nitrification, with similar rates (17.2-18.9 mg kgp# 14 daysp#) among the four sampling areas. In the second part of the study, we emplaced soil cores that either allowed root in-growth or excluded roots to evaluate how roots directly affect soil CO and CH. The three plant species had similar amounts of root growth (ca 290 g mpo yearp#). Fungal biomass was similar in soils with root in-growth versus root exclusion, regardless of dominant plant species. Rates of soil CO production did not differ with root in-growth versus root exclusion, and added glucose increased CO production rates by only 35%. Root in-growth did lead to greater rates of CH production; albeit, addition of glucose had much greater effect on CH production (1.24 nmol kgp# sp#) compared with controls without added glucose (0.058 nmol kgp# sp#). Our data revealed relatively few subtle differences in soil characteristics and processes associated with different plant species; albeit, roots had little effect, even inhibiting some microbial processes. This research highlights the need for both field and experimental studies in long-established monocultures of plant species to understand the role of plant biodiversity in soil function.
机译:植物会为土壤提供土壤微生物所需的有机碳(OC)化合物,但是单个植物物种(或具有独特性状的植物)是否如此独特尚不确定。我们评估了湿地中的土壤微生物过程,在该湿地中,不同植物物种(香蒲-香蒲-;紫色的珍珠菜-千屈菜-L;芦苇金丝雀-ala草-L)占主导地位。我们还建立了一个去除植物芽的实验区。 ala草地区的酸性土壤pH值更高(7.08 vs.7.27-7.57),土壤有机质含量更高(19.0%vs. 9.0-11.5%),CO生成速度最慢(0.10 vs. 0.21-0.46 omol kgp #sp#)和CH(0.040对0.054-0.079 nmol kgp#sp#)。氮循环以净硝化作用为主,在四个采样区中氮的循环速率相似(17.2-18.9 mg kgp#14天p#)。在研究的第二部分中,我们放置了允许根系向内生长或排除根系的土壤核心,以评估根系如何直接影响土壤CO和CH。这三种植物的根生长量相似(约290 g mpo年p#)。根系生长与根系排斥的土壤中真菌生物量相似,而与优势植物种无关。根部生长与根部排斥相比,土壤CO产生速率没有差异,添加葡萄糖可使CO产生速率仅增加35%。根系的生长确实导致了CH产生率的增加。尽管添加葡萄糖与未添加葡萄糖的对照(0.058 nmol kgp#sp#)相比,对CH的产生具有更大的影响(1.24 nmol kgp#sp#)。我们的数据表明,与不同植物物种相关的土壤特征和过程的细微差别不大。虽然,根几乎没有影响,甚至抑制了某些微生物过程。这项研究强调了对已建立的植物物种单一栽培进行田间研究和实验研究的必要性,以了解植物生物多样性在土壤功能中的作用。

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