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Elevated carbon dioxide increases soil nitrogen and phosphorus availability in a phosphorus-limited Eucalyptus woodland

机译:二氧化碳含量升高会限制磷含量有限的桉树林地的土壤氮和磷的利用率

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Free-air CO2 enrichment (FACE) experiments have demonstrated increased plant productivity in response to elevated (e)CO2, with the magnitude of responses related to soil nutrient status. Whilst understanding nutrient constraints on productivity responses to eCO(2) is crucial for predicting carbon uptake and storage, very little is known about how eCO(2) affects nutrient cycling in phosphorus (P)-limited ecosystems. Our study investigates eCO(2) effects on soil N and P dynamics at the EucFACE experiment in Western Sydney over an 18-month period. Three ambient and three eCO(2) (+150ppm) FACE rings were installed in a P-limited, mature Cumberland Plain Eucalyptus woodland. Levels of plant accessible nutrients, evaluated using ion exchange resins, were increased under eCO(2), compared to ambient, for nitrate (+93%), ammonium (+12%) and phosphate (+54%). There was a strong seasonality to responses, particularly for phosphate, resulting in a relatively greater stimulation in available P, compared to N, under eCO(2) in spring and summer. eCO(2) was also associated with faster nutrient turnover rates in the first six months of the experiment, with higher N (+175%) and P (+211%) mineralization rates compared to ambient rings, although this difference did not persist. Seasonally dependant effects of eCO(2) were seen for concentrations of dissolved organic carbon in soil solution (+31%), and there was also a reduction in bulk soil pH (-0.18 units) observed under eCO(2). These results demonstrate that CO2 fertilization increases nutrient availability - particularly for phosphate - in P-limited soils, likely via increased plant belowground investment in labile carbon and associated enhancement of microbial turnover of organic matter and mobilization of chemically bound P. Early evidence suggests that there is the potential for the observed increases in P availability to support increased ecosystem C-accumulation under future predicted CO2 concentrations.
机译:自由空气CO2浓缩(FACE)实验表明,随着(e)CO2浓度升高,植物生产力提高,其响应幅度与土壤养分状况有关。尽管了解营养素对生产力对eCO(2)的响应的限制对于预测碳的吸收和储存至关重要,但对eCO(2)如何影响磷(P)受限的生态系统中的营养素循环了解甚少。我们的研究调查了eCO(2)对西悉尼EucFACE实验在18个月内对土壤氮和磷动力学的影响。在P限制的成熟坎伯兰平原桉树林中安装了三个环境环和三个eCO(2)(+ 150ppm)FACE环。与环境相比,在eCO(2)下,使用离子交换树脂评估的植物可利用营养素的水平相对于环境而言增加了,其中硝酸盐(+ 93%),铵盐(+ 12%)和磷酸盐(+ 54%)。在春季和夏季,在eCO(2)下,对响应的响应具有强烈的季节性,特别是对磷酸盐而言,导致相对于N的可用P的刺激相对较大。在实验的前六个月中,eCO(2)还与更快的养分周转率相关,与环境环相比,更高的N(+ 175%)和P(+ 211%)矿化率,尽管这种差异并没有持续。对于土壤溶液中溶解的有机碳浓度(+ 31%),可以看到eCO(2)的季节性依赖性。在eCO(2)下,土壤总体pH值也降低了(-0.18单位)。这些结果表明,CO 2施肥可以增加磷在有限磷土壤中的养分利用率,尤其是磷肥,这可能是通过增加地下植物对不稳定碳的投资以及相关有机物微生物周转率的提高和化学结合磷的动员而实现的。早期证据表明,是在未来预测的CO2浓度下观测到的P利用率增加的潜力,以支持增加的生态系统C积累。

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