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41.
Tommaso Chiti Giacomo Certini Lucia Perugini Giovanni Mastrolonardo Dario Papale Riccardo Valentini 《Regional Environmental Change》2011,11(2):371-376
The purpose of the present work is to asses the possibility of detecting changes in soil organic carbon (SOC) at the end of
the 5-years of the first Commitment Period (CP) of the Kyoto Protocol of the United Nation’s Framework Convention on Climate
Change (1 January, 2008–31 December, 2012), by both direct measurement and the use of an opportunely evaluated SOC model,
CENTURY. The investigated soil is young, developed since 28 years on virtually C-free spoil banks and under the influence
of two managed forest stands, one a mix of English oak (Quercus robur L.) and Italian alder (Alnus cordata Loisel.) and the other pure English oak. The SOC stock of either stand was monitored since the time the stands were planted
in 1981, and it was used together with other parameters for the model evaluation, while the future projections for the end
of the first (2012) and second (2017) CP were made according to two extreme IPCC climatic scenarios: A1F1, the most dramatic,
and B2, among the less impacting. Direct SOC measurements performed at the beginning and at the end of a time frame equivalent
to a commitment period (2004–2008) had not shown significant variations in either stands. Compared to the 2008 SOC stock,
in both stands the model shows variations at the end of the first CP from 0.7 to 1.8 Mg C ha−1 for the A1F1 scenario and from 0.3 to 1.7 Mg C ha−1 for the B2. These variations are within the standard deviations of the C stocks measured in 2008. On the contrary, at the
end of the second CP, the modelled SOC increments range from 2.5 to 3.6 Mg C ha−1 (A1F1) or from 1.9 to 3.4 Mg C ha−1 (B2), indicating the possibility to detect the SOC changes by direct measurement, since the values well agree with the minimum
detectable variation estimated for both sites in 3.3–4.5 Mg C ha−1. This work shows that SOC stock changes measured directly in the field can be minimal at the end of both CPs, and that CENTURY
well simulates the SOC dynamics of the stands. The use of such a model, validated at long-term experimental sites, hence represents
an effective tool for estimating future changes in SOC amounts in support of direct measurements when a short period of time,
such as the CP, is considered. 相似文献
42.
Specchiulli Antonietta Scirocco Tommaso D’Adamo Raffaele Cilenti Lucrezia Fabbrocini Adele Cassin Daniele Penna Pierluigi Renzi Monia Bastianoni Simone 《Journal of Coastal Conservation》2016,20(5):363-374
Phytoplankton and benthic vegetation biomass undergoes spatial-temporal changes in relation to their life cycle, but also to meteorological conditions, physical-chemical variables, organic input and internal dynamism. The main aim of this work was to observe the effect of all environmental variables on the vegetative dynamic process in a protected zone of a Mediterranean costal lagoon (Lesina lagoon, SE Italy). Seven samplings were performed from 2010 to 2012 at 30 sites for nutrient and chlorophyll analyses, while TOC measurements and wet biomass evaluation were performed at 10 sites. Temperature, salinity and oxygen saturation were also measured by multiparametric probe and a visual census for vegetation was performed. Sites close to freshwater inflow were characterized by lower temperature and salinity, and high nitrate, with maxima of 191.05 μM in May 2010 and more than 250 μM in October 2010. Silicates drastically decreased from May 2010 (87.57 μM) to July 2010 (6.15 μM) and increased again in October (74.99 μM). Chl a concentrations were not on average higher than 6 mg m?3, but peaks of 20 mg m?3 were observed during May 2011 and May 2012. Benthic vegetation wet biomass collected in 2010 was approximately twice that collected in 2012, with a maximum of 27,554 g m?2 and a dominance of macroalgae (70 % in May 2010 and 40 % in August 2010). During period 2010, a simultaneous and drastic decreasing of both mean values of wet biomass and chl a was observed from May to October 2010. During period 2012 a shift of vegetation biomass was shown from May (phytoplankton prevalence) to August 2012, with angiosperm prevalence (more than 30 %). 相似文献
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