| Records |
| Author |
Kopacz, M.; Twardy, S. |
Title  |
Spatial Modeling as a Tool Supporting the Management of Catchment Area of Retention Reservoir |
Type |
Conference Article |
| Year |
2014 |
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LiveM; CropM |
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VII Conference on Environmental Protection and Engineering - Sustainable Development held at AGH University of Science and Technology in Krakow, 2014-06-26 to 2014-06-27 |
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no |
| Call Number |
MA @ admin @ |
Serial |
2569 |
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| Author |
Kopacz, M.; Twardy, S. |
| Title |
Spatial modeling as a tool supporting the management of catchment area of retention reservoir |
Type |
Journal Article |
| Year |
2014 |
Publication |
Polish Journal of Environmental Studies |
Abbreviated Journal |
Pol. J. Environ. Stud. |
| Volume |
23 |
Issue |
3a |
Pages |
53-57 |
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English |
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CropM, LiveM |
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no |
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MA @ admin @ |
Serial |
4628 |
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| Author |
Kipling, P.; Saetnan, R.; van den Pol-van Dasselaar, A.; Scollan, N.D. |
| Title |
SOLID project workshop and annual meeting, MTT Finland |
Type |
Conference Article |
| Year |
2014 |
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LiveM |
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Overview of LiveM, 2014-05-21 to 2014-05-23 |
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no |
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MA @ admin @ |
Serial |
2536 |
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| Author |
Ghaley, B.B.; Porter, J.R.; Sandhu, H.S. |
| Title |
Soil-based ecosystem services: a synthesis of nutrient cycling and carbon sequestration assessment methods |
Type |
Journal Article |
| Year |
2014 |
Publication |
International Journal of Biodiversity Science, Ecosystem Services & Management |
Abbreviated Journal |
International Journal of Biodiversity Science, Ecosystem Services & Management |
| Volume |
10 |
Issue |
3 |
Pages |
177-186 |
| Keywords |
ecosystem functions; litter decomposition; mineralisation; assessment methodologies; stoichiometry |
| Abstract |
Among the soil-based ecosystem services (ES), nutrient cycling and carbon sequestration have direct influence on the biogeochemical cycles and greenhouse gas emissions affecting provision of other ES that support human existence. We reviewed methods to assess the two key ES by identifying their strengths and weaknesses and have made suggestions for using appropriate methods for better understanding of the ecosystem functions for the provision of ES. Relevant papers for the review were chosen on the basis of (i) diversity of studies on the two key ES in different ecosystems, (ii) methodologies applied and (iii) detailed descriptions of the trial locations in terms of vegetation, soil type, location and climatic information. We concluded that (i) elemental stoichiometrical ratios could be a potential approach to assess the health of ecosystems in terms of provision of the two ES discussed, (ii) stoichiometric imbalances need to be avoided between the supply and the demand of the nutrients to maintain the ES provision in terrestrial ecosystems and (iii) stoichiometric ratios can act as a management tool at a field, farm and at landscape level, to complement other compositional biodiversity and functional diversity approaches to ensure sustainable provision of ES. |
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2151-3732 2151-3740 |
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| Notes |
CropM, ftnotmacsur |
Approved |
no |
| Call Number |
MA @ admin @ |
Serial |
4522 |
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| Author |
Patil, R.H.; Laegdsmand, M.; Olesen, J.E.; Porter, J.R. |
| Title |
Soil temperature manipulation to study global warming effects in arable land: performance of buried heating-cable method |
Type |
Journal Article |
| Year |
2014 |
Publication |
Environment and Ecology Research |
Abbreviated Journal |
Environment and Ecology Research |
| Volume |
1 |
Issue |
4 |
Pages |
196-204 |
| Keywords |
Climate Change; Climate Manipulation; Soil Warming; Heating Cables; Soil Temperature; Agro-Ecosystems |
| Abstract |
Buried heating-cable method for manipulating soil temperature was designed and tested its performance in large concrete lysimeters grown with the wheat crop in Denmark. Soil temperature in heated plots was elevated by 5℃ compared with that in control by burying heating-cable at 0.1 m depth in a plough layer. Temperature sensors were placed at 0.05, 0.1 and 0.25 m depths in soil, and 0.1 m above the soil surface in all plots, which were connected to an automated data logger. Soil-warming setup was able to maintain a mean seasonal temperature difference of 5.0 ± 0.005℃ between heated and control plots at 0.1 m depth while the mean seasonal rise in soil temperature in the top 0.25 m depth (plough layer) was 3℃. Soil temperature in control plots froze (≤ 0℃) for 15 and 13 days respectively at 0.05 and 0.1 m depths while it did not in heated plots during the coldest period (Nov-Apr). This study clearly showed the efficacy of buried heating-cable technique in simulating soil temperature, and thus offers a simple, effective and alternative technique to study soil biogeochemical processes under warmer climates. This technique, however, decouples below-ground soil responses from that of above-ground vegetation response as this method heats only the soil. Therefore, using infrared heaters seems to represent natural climate warming (both air and soil) much more closely and may be used for future climate manipulation field studies. |
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CropM, ftnotmacsur |
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no |
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MA @ admin @ |
Serial |
4632 |
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