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Proceedings of International Workshop on valuation and Sustainable Management of Soil Carbon Sequestration in Asian Countries |
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Sunday, 26 September 2010 14:11 |
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Soil is not only important for supporting the livelihood of the human beings, fauna and flora, but also an important storage of carbon. The soil organic carbon (SOC) pool is about 3.3 times the amount of the atmospheric C pool and 4.5 times the amount of the biotic C pool. SOC affects the soil fertility and in turns determine the plant and animal biomass. The SOC pool to 1m depth ranges from 30 Mg ha-1 in arid climates to 800 Mg ha-1 in organic soils in cold regions as well as in the tropical peatland, with a predominant range of 50 to 150 Mg ha-1 in mineral soils. The SOC pool represents a dynamic equilibrium of gains and losses of C in soil system. Conversion of natural forest to agricultural ecosystems causes depletion of the SOC pool by as much as 60% in soils of temperate regions and 75% or more in cultivated soils of the tropics. Management of degraded soils may restock the soil carbon and, to some extent, mitigate the global warming and climate changes. This proceedings is a compilation of invited papers presented in the international workshop on Evaluation and Sustainable Management of Soil Carbon Sequestration in Asian Countries, held at the IPB International Convention Center, Bogor, Indonesia, from 28 to 29 September, 2010. The invited papers cover ranges of topics from soil database and mapping of SOC, soil management and spatial and temporal changes of SOC by different land uses, as well as properties and dynamics of carbon in peatland areas.
Table of Content
Foreword / Inside Cover / Welcome Address / Welcome and Opening Address
Soil Carbon Stocks in the U.S.: Current Data and Future Inventories L.T. West, S.W. Waltman, S. Wills, T.G. Reinsch, E.C. Benham, C.S. Smith, R. Ferguson 1
Estimation of Soil Carbon Stock Changes in Japanese Agricultural Soils using National Resources Inventory Yusuke Takata 15
Chronological Changes of Soil Carbon Stock in Korea Yoo-Hak Kim, Seong-Soo Kang, Myung-Sook Kim 29
Use of Remote Sensing in Assessment of Soil and Ecosystem Carbon Status Yoshio Inoue 39
Indonesian Soil Data Base and Predicted Stock of Soil Carbon Rizatus Shofiyati, Irsal Las, Fahmuddin Agus 73
Organic Carbon Storage and Management Strategies of the Forest Soils Based on the Forest Soil Survey Database in Taiwan Chen-Chi Tsai, Zueng-Sang Chen, Zeng-Yei Hseu, Chin-Tzer Duh, Horng-Yuh Guo 85
Monitoring Spatio-Temporal Changes of Soil Carbon in Java Using Legacy Soil Data Yiyi Sulaeman, Budiman Minasny, Alex. B. McBratne 103
Aggregate Stability and Soil Carbon Storage as Affected by Different Land Use Practices Kyung-Hwa Han, Sang-Geun Ha, Byoung-Choon Jang 113
Organic Carbon Storage and Management Strategies of the Rural Soils on the Basis of Soil Information System in Taiwan Shih-Hao Jien, Zeng-Yei Hseu, Horng-Yuh Guo, Chen-Chi Tsai, Zueng-Sang Chen 125
Soil Carbon Sequestration and Greenhouse Gases Mitigation in Selected Ecosystems in the Philippines Rodolfo O. Ilao, Edilberto D. Salang, Januel P. Floresca 139
Soil Management for Maximizing Carbon Sequestration in Thailand Sathaporn Jaiarree 153
Soil Carbon Stocks in Sarawak, Malaysia E. Padmanabhan, H. Eswara, P.F. Reich 167
Carbon in Vietnamese soils and experiences to improve carbon stock in soil Pham Quang Ha 175
Distribution, Properties, and Carbon Stock of Indonesian Peat Land Wahyunto, Ai Dariah, Fahmuddin Agus 187
Properties of Indonesian Peat in Relation to the Chemistry of Carbon Emission Supiandi Sabiham 205
Carbon budget and management strategies for conserving carbon in peatland: Case study in Kubu Raya and Pontianak Districts, West Kalimantan, Indonesia Fahmuddin Agus, Wahyunto, Ai Dariah, Prihasto Setyanto, I.G. Made Subiksa, Eleonora Runtunuwu, Erni Susanti, Wahyu Supriatna 217
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Tuesday, 24 August 2010 14:48 |
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Root respiration interferes with peat CO2 emission measurement
Fahmuddin Agus, Etik Handayani, Meine van Noordwijk, Kamarudin Idris, Supiandi Sabiham
Abstract
Root respiration and microbial decomposition release CO2 from peatland. Mixture between these two measurements causes an over-estimation of greenhouse gas contribution, because CO2 produced by the former is offset by atmospheric CO2 removal during photosynthesis. We separated the two components by measuring, from closed chambers, the CO2 emission from the rooted (R) and non-rooted (NR) zones of peatland planted to oil palm. Three pieces of roots were channelled through a 5 cm hole into each of the grounded part of the R chamber. Emitted CO2 was captured by 30-cm diameter and 30-cm tall PVC gas chambers, sampled using 10 ml syringes, and measured using gas chromatography. The measurements were conducted in Aceh, Sumatra in the early rainy season (Oct-Nov 2008). We found that CO2 emitted from the NR chambers was about 62% of that of the R chamber, indicating a significant contribution of the root in producing CO2. The average amount of emitted CO2 from these 1, 5 and 10 year oil palm soils ranged from 18 to 24 t/ha/yr. Capturing both the R and NR zones in CO2 emission measurement is advisable, but under limited resources, the NR zone should be prioritised.
Key Words: Peat, root respiration, microbial decomposition, CO2 emissions
Paper presented at 19th World Congress of Soil Science, Soil Solutions for a Changing World. 1-6 August 2010. Brisbane. Australia. Published on DVD.
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Monday, 07 June 2010 16:53 |
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Nutrient Balance and Vegetable Crop Production as Affectedby Different Sources of Organic Fertilizers
Fahmuddin Agus, Diah Setyorini, Wiwik Hartatik, Sang-Min Lee, Jwa-Kyung Sung, and Jae-Hoon Shin
ABSTRAK
Understanding the net nutrient balance in a farming system is crucial in assessing the systems sustainability. We quantified N, P and K balances under vegetable organic farming in a Eutric Hapludand in West Java, Indonesia in five planting seasons from 2005 to 2007. The ten treatments and three replications, arranged in a completely randomized block design, included single or combined sources of organic fertilizers: barnyard manure, composts or green manures. The organic matter rates were adjusted every planting season depending on the previous crop responses. The results showed that the application of 20 t ha-1 barnyard manure per crop resulted in positive balances of N, P, and K, except in the second crops of 2006 where potassium balance were -25 to -11 kg ha-1 under the treatments involving cattle barnyard manure, because of low K content of these treatments and high K uptake by Chinese cabbage. Application of 20 to 25 t ha-1 of plant residue or 5 t ha-1 of Tithonia compost also resulted in a negative K balance. Soil available P increased significantly under 25 t ha-1 barnyard manure and that under chicken manure had the highest available P. Accordingly, chicken barnyard manure gave the highest crop yield because of relatively higher N, P and K contents. Plant residues gave the lowest yield due to the lowest nutrient content among all sources. Reducing the use of barnyard manure to 12.5 t ha-1 and substituting it with Tithonia compost, Tithonia green manure or vegetable plant residue compost gave insignificantly different yield compared to the application of 25 t ha-1 barnyard manure singly. In the long run, application of 25 t ha-1 cattle, goat, and horse manure or about 20 t ha-1 chicken manure is recommendable for sustaining the fertility of this Andisol for vegetable production.
Key words: Nutrient balance, vegetable crops, barnyard manure, organic farming, Andisol Papers published in Korean Journal of Soil Science Fertilizer. 42 (1). 1-13 (2009) |
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