scholarly journals Checking the progress of using the static chamber method for the measurement of greenhouse gases in Latin America

2021 ◽  
pp. 1-13
Author(s):  
Fernanda Figueiredo Granja Dorilêo Leite ◽  
Bruno José Rodrigues Alves ◽  
Gabriel Nuto Nóbrega ◽  
Renato Campello Cordeiro ◽  
Fernando Vieira Cesário ◽  
...  
2021 ◽  
Author(s):  
Graciela B. Raga

I have the pleasure to introduce this new issue of Atmósfera which this year, its 33rd since being founded by Dr. Julian Adem, has once again started publishing systematically 8 papers per number. In particular, in this issue we have the great fortune to share editing responsibilities with Dr. Luisa Molina, a well renowned and much celebrated scientist and editor. The papers edited by her relate to issues associated with emissions of greenhouse gases and to methodologies to estimate them in Latin America. These papers provide methods that are very relevant to accurately measure emissions that aid in the estimates of national inventories and provide better tools for designing mitigation strategies.


2019 ◽  
Vol 10 (3) ◽  
pp. 181-191 ◽  
Author(s):  
Kayaba Haro ◽  
Issoufou Ouarma ◽  
Bernard Nana ◽  
Antoine Bere ◽  
Guy Christian Tubreoumya ◽  
...  

Atmosphere ◽  
2020 ◽  
Vol 11 (3) ◽  
pp. 286
Author(s):  
Renata Gruca-Rokosz

Research carried out in the years 2009–2011 and 2018–2019 sought to determine the magnitudes of fluxes of methane (CH4) and carbon dioxide (CO2) from the surfaces of three eutrophic reservoirs in SE Poland. The “static chamber” method was deployed at five or six stations located along the reservoirs, where the water column at its deepest slightly exceeds 2 m. Obtained values for the fluxes of CH4 varied across a wide (0–2513.48 mmol·m−2·d−1) range, with many of these values therefore exceeding those characteristics for large tropical reservoirs. The reservoirs studied were not found to differ significantly in terms of average CH4 flux, however. Where obtained values for CO2 fluxes in the range from −10.96 to 621.69 mmol·m−2·d−1 were concerned, most fell within the range given for temperate-zone reservoirs, while differences between reservoirs were noted for average values in this case.


2018 ◽  
Vol 9 (1) ◽  
pp. 10
Author(s):  
Anggri Hervani ◽  
Rina Kartikawati ◽  
Miranti Ariani ◽  
Prihasto Setyanto

<p><em>Expansion of sugarcane areal to support enhancement production and fulfilment target of self-sufficiency for national sugar should be conducted to see environment impact, particularly related to greenhouse gases emission. The objective of this study was to figure out N<sub>2</sub>O emission from conventional sugarcane plantation by farmer in rainfed area. The observation of N<sub>2</sub>O gas was carried out in sugarcane plantation in Sidomukti Village, Jaken District, Pati, Central Java. Sampling of N<sub>2</sub>O gas was conducted by <em>close chamber method</em>. The study showed that maximum fluxes of sugarcane plantation before and after fertilizer application are 4.011 and 223 µg N<sub>2</sub>O m<sup>-2</sup> day<sup>-1</sup>. Meanwhile, after fertilizer application the maximum and minimum fluxes of N<sub>2</sub>O are 6.408 and 25 µg N<sub>2</sub>O m <sup>-2</sup> day<sup>-1</sup>. N<sub>2</sub>O emission from sugarcane plantation recorded in rainfed area as 4.21 ± 2.53 kg N<sub>2</sub>O ha<sup>-1</sup> year<sup>-1</sup> with potential of global warming number as 1.31 ton CO<sub>2</sub>-e per hectar per year.</em></p><p><em><br /></em></p><p><strong>Emisi N2O dari Pertanaman Tebu di Lahan Tadah Hujan</strong></p><p>Perluasan areal tanam tebu untuk mendukung peningkatan produksi dan pemenuhan target swasembada gula nasional sudah dianggap perlu untuk melihat dampak lingkungan khususnya mengenai evaluasi emisi gas rumah kaca dari pertanaman tebu. Tujuan dari penelitian ini adalah untuk mengetahui emisi gas N<sub>2</sub>O dari sistem pertanaman tebu secara konvensional petani di lahan tadah hujan. Pengamatan gas N<sub>2</sub>O dilakukan pada lahan perkebunan tebu di desa Sidomukti Kecamatan Jaken Kabupaten Pati Provinsi Jawa Tengah. Pengambilan sampel N<sub>2</sub>O menggunakan metode sungkup tertutup. Hasil penelitian menunjukkan bahwa fluks maksimum pada pertanaman tebu sebelum pemupukan sebesar 4,011 µg N<sub>2</sub>O m <sup>-2</sup> hari<sup>-1</sup> dan fluks minimum sebesar 223 µg N<sub>2</sub>O m <sup>-2</sup> hari<sup>-1</sup>, sedangkan fluks maksimum setelah pemupukan sebesar 6,408 µg N<sub>2</sub>O m <sup>-2</sup> hari<sup>-1 </sup>dan fluks minimum sebesar 25 µg N<sub>2</sub>O m <sup>-2</sup> hari<sup>-1</sup>. Emisi N<sub>2</sub>O pertanaman tebu sebesar 4.21 ± 2.53 kg N<sub>2</sub>O ha<sup>-1</sup>tahun<sup>-1</sup> dengan nilai potensi pemanasan global sebesar 1.31 ton CO<sub>2</sub>-e per hektar per tahun.</p>


2016 ◽  
Vol 7 (2) ◽  
pp. 56-65
Author(s):  
M V Glagolev ◽  
I E Terentieva

The paper discusses several controversial points from thesis of Nikolai Andreevich Shnyrev «Regime investigations and estimate of gas exchange on the soil-atmosphere interface (methane fluxes from “Muhrino” wetland, West Siberia»). These points concern mainly previous estimates of regional methane emission from West Siberian wetlands, in particular, by Glagolev’s scientific group. The paper shows that “large variability of estimates as well as large disbalance in carbon cycle”, which was claimed in thesis to prove its relevance, contradict to modern investigations of the problem. We also discuss several methodological problems of static chamber method. In particular, it was proved that difference between methane emissions in the light and in the dark is negligible. In addition, we showed that N.A. Shnyrev’s suggestion on improvement the accuracy of static chamber method by reduction of chamber volume is unreasonable. Finally, we discuss if linearity of methane concentration dynamic is necessary for methane flux calculations.


Author(s):  
Hossein Ali Alikhani ◽  
Saeed Karbin ◽  
Babak Moteshare Zadeh

Conservation Agriculture (CA) alters soil properties and microbial processes compared to conventional agriculture. These changes can affect soil-atmosphere greenhouse gas (GHG) fluxes. In this overview, we summarized the results of global literature and the gaps in measuring and understanding of GHG fluxes in CA systems and conventional agriculture. Some studies compared soil carbon sequestration and soil respiration in conservation agriculture and no-tillage system with conventional agriculture and the results were not consistent in all experiments. Interactions between CA pillars and soil factors such as soil moisture, temperature, texture can determine the rate of respiration rate and soil-atmosphere CO2 fluxes. The majority of studies reported larger N2O emissions in no-tillage treatment compared with conventional tillage while some other studies reported no difference between no-tillage and conventional tillage systems. In the majority of CA studies, there is lack of required information which is necessary to understand the mechanisms and processes that affect soil GHG fluxes. Determining factors like climate, amount of plant residues, soil type, crop types included in crop rotation and cover crops and duration of the study are not considered. Static chamber method was used for measuring soil-atmosphere GHG fluxes in the majority of studies. Spatial and temporal changes in GHG flux rates are high and missing part of highly episodic events by using static chamber method may result over- or under-estimation in flux balance calculation. Applying standard techniques for measuring continuous fluxes can help to calculating accurate GHG balance.


2011 ◽  
Vol 62 (6) ◽  
pp. 811-821 ◽  
Author(s):  
P. E. Levy ◽  
A. Gray ◽  
S. R. Leeson ◽  
J. Gaiawyn ◽  
M. P. C. Kelly ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document