Journal Search Engine
Search Advanced Search Adode Reader(link)
Download PDF Export Citaion korean bibliography PMC previewer
ISSN : 2287-5824(Print)
ISSN : 2287-5832(Online)
Journal of The Korean Society of Grassland and Forage Science Vol.35 No.3 pp.251-256
DOI : https://doi.org/10.5333/KGFS.2015.35.3.251

Annual Greenhouse Gas Removal Estimates of Grassland Soil in Korea

Sang Hack Lee*, Hyung Soo Park, Young-Jin Kim, Won Ho Kim, Jung Jong Sung
National Instisute of Animal Science, Rural Development Administration, cheonan 330-801, Korea
*Correspondingauthor:Sang Hack Lee, National Institute of Animal Science RDA, Cheonan 330-801, Korea. Tel: +82-41-580-6773, Fax: +82-41-580-6757, E-mail: esh79@korea.kr
August 31, 2015 September 4, 2015 September 8, 2015

Abstract

The study was conducted to determine greenhouse gas (GHG) inventories in grasslands. After ‘Low Carbon Green Growth’ was declared a national vision on 2008, Medium-term greenhouse gas reduction was anticipated for 30% reduction compared to Business As Usual (BAU) by 2020. To achieve the reduction targets and prepare to enforce emissions trading (2015), national GHG inventories were measured based on the 1996 Intergovernmental Panel on Climate Change Guidelines (IPCC GL). The national Inventory Report (NIR) of Korea is published every year. Grassland sector measurement was officially added in 2014. GHG removal of grassland soil was measured from 1990 to 2012. Grassland area data of Korea was used for farmland area data in the 「Cadastral Statistical Annual Report (1976~2012)」 . Annual grassland area corresponding to the soil classification was used Soil classification and commentary in Korea (2011) . Grassland area was divided into ‘Grassland remaining Grassland’ and ‘Land converted to Grassland’. The accumulated variation coefficient was assumed to be the same without time series changes in grassland remaining grassland. Therefore, GHG removal of soil carbon was calculated as zero (0) in grassland remaining grassland. Since the grassland area increases constantly, the grassland soil sinks constantly . However, the land converted to grassland area continued to decrease and GHG removal of soil carbon was reduced. In 2012 (127.35Gg CO2), this removal decreased by 76% compared to 1990 (535.71 Gg CO2). GHG sinks are only grasslands and woodlands. The GHG removaled in grasslands was very small, accounting for 0.2% of the total. However, the study provides value by identifying grasslands as GHG sinks along with forests.


초록


    Rural Development Administration
    No. PJ010284022015

    I.INTRODUCTION

    The ecological importance of grasslands has mainly been emphasized in the field of biodiversity. Recently, reports signifies lot of attention to carbon storage in grassland with regard to climate change. Grassland soil carbon stocks amount to at least 10% of the global total (Eswaran et al. 1993), but other sources estimate up to 30% of world soil carbon (Anderson 1991). This concern of grassland is further increased by land use, land use change, and forestry (LULUCF).

    The LULUCF sector deals with GHG emissions and removals resulting from land use such as forestry activities and land-use change. The land-use category is divided into six kinds such as forest land, cropland, grassland, wetlands, settlements, other land by Good Practice Guidance (GPG) of IPCC. Although forestry is the most important in terms of carbon storage. which can store large amounts of organic matter in cropland and grassland soil (Post and Kwon, 2000).

    In Korea, After ‘Low Carbon Green Growth’ was declared a national vision on 2008, Medium-term greenhouse gas reduction was anticipated for 30% reduction compared to Business As Usual (BAU) by 2020. To achieve the reduction targets and prepare to enforce emissions trading (2015), national GHG inventories were measured based on the 1996 IPCC GL. Every year, for preparing the national GHG inventory, National Greenhouse Gas Inventories Measurement, Reporting, Verification (MRV) and National Inventory Report (NIR) has been written based on the IPCC 1996 GL, GPG 2000, GPG 2003.

    The national GHG inventory details national GHG emissions in energy, industrial processes, agriculture, LULUCF and waste sectors in accordance with IPCC GL. LULUCF sector measure all anthropogenic GHG emissions of managed land. LULUCF is the only sector to measure the emissions and removals. Grasslands belong to the LULUCF sector with forest land, cropland, wetlands, settlements, other land. Grassland sector measurement was officially added in 2014.

    II.MATERIALS AND METHODS

    1.Grassland area

    Grassland area data of Korea is used farmland area data in cadastral statistical annual report from 1976 to 2012. Annual grassland area of the soil classification are divided into jeju province and other. Except for jeju, the national rate of soil types are LAC soil 94.5%, sandy soil 5.5% (Kang et al, 2011). The nationwide area was calculated according to rate of soil types.

    All grassland soil of jeju was regarded as a volcanic ash soil. Grassland area of jeju was estimate farmland area data in cadastral statistical annual report.

    Depending on the default inventory storage period of 20 years of the IPCC GL, time series completeness of grassland data does not exist in the Korea (1970~1975) were supplemented through trend extrapolation.

    LULUCF divided land use into six purpose categories and computes the change in emissions, according to whether the land uses “maintain” or “change” in purpose. So, this section divides grassland into two subcategories, “Grassland remaining Grassland” and “Land converted to Grassland”, and describes them separately in the following subsections. The grassland remaining grassland area is the smaller area as compared to in the inventory year and 20 years ago. Land converted to grassland is larger than 20 years ago.

    Japan classifies its national land into six categories forest land, cropland, grassland, wetlands, settlements, and other land and subdivides each of them into two subcategories by distinguishing them on the basis of whether or not land conversion has been occurred, in accordance with the 2006 IPCC GL. It also uses 20 years, a default value in the 2006 IPCC GL, when distinguishing the land conversion (Ministry of the Environment, Japan, 2015)

    2.Emissions and removals coefficient

    To calculate the Soil Organic Carbon Stocks (SOC) of grassland, it was used that default reference soil organic carbon stocks (SOCREF) provided from IPCC GL according to climate and land type.

    Climate of Korea belongs to warm temperate and moist climate. Total soil in Korea except for jeju are classified into low activity clay (LAC) and sandy soils. All grassland soil of jeju was regarded as a volcanic ash soil. Soil type area are LAC: 70.6%, Sandy soil: 4.1, Volcanic ash soil in Jeju: 23.5% (Kang et al., 2011). The amount of SOC was calculated by applying the accumulated variation coefficient of 1.0 and area of soil type.

    Accumulated variation coefficient was applied that basic value of GPG-LULUCF depending separated by method of land utilization, tillage methods and organic matter inputs. Accumulated variation coefficient of FLU depending was separated by land utilization. Type of land utilization change is applied that basic value of GPG-LULUCF is 1.0 for the entire grassland and the whole climate system. Accumulated variation coefficient of FMG by grassland management system was applied that 1.0 (continue to be managed without damaging grasslands). Accumulated variation coefficient of FI by the amount of organic matter utilization was applied 1.0 on the basic amount used in grassland of Korea. Table. 1

    3.Method of measurement

    CO2 emissions and removal of grassland sector in Korea was applied on the basis value of representing the grassland soil conditions in Korea from GPG-LULUCF. Because area of organic soil was too small, organic grasslands were not existed. Carbon stock variation of the land of maintained as grassland was calculated zero (0) in accordance with the KGFS-35-251_Image.gif organic matter accumulated variation coefficient of the same trial without time series change by land utilization, management system and organic matter utilization.

    III.RESULTS AND DISCUSSION

    Basic data of land use classification uses statistical data such as cadastral statistics, agriculture census. Grassland sector should take advantage of pasture area on the cadastral statistics.

    In some cases, estimate the area of land conversion using the fair value ratio, use interpolation and trend extrapolation because lack of statistic data (Ministry of the Environment, Japan, 2015). There is no pasture area from 1970 to 1975 on the cadastral statistics. Therefore, the trend extrapolation method was used from 1970 to 1975. However, the grassland area was reduced sharply during two years (1976 ~ 1977), it could not calculate from 1970 to 1975. so, 1976 and 1977 was added to the trend extrapolation (Table 2).

    According to grassland area statistics, total amount of grassland area is constantly increased (Fig. 1). In 2012, Korea’s grassland area was about 58,019 ha. But, increasing rate is gradually reduced. Between 2011 and 2012, decreased from 58,179 ha to 58,019 ha.

    Based on the soil maintenance period of 20 years of the IPCC GL and subdivide annual grassland area. As the starting point for each inventory year, the grassland area divides grassland remaining grassland area (Table 3) and land converted to grassland area (Table 4) for 23 years. Table 5

    Grassland remaining grassland is remaining grassland during the past 20 years. it is an area 20 years ago from their inventory year.

    Land converted to grassland occurred in the lands that were converted from other land-use categories to grassland within the past 20 years. it was increased area more than 20 years ago. Because of this grassland area increases every year, grassland area replaced by other land can be assumed to be non-existent. But, land converted to grassland area is continuously decreased.

    1Greenhouse gas removal

    As the starting point for each inventory year, the grassland area was divided into grassland remaining grassland area and land converted to grassland area for 23 years.

    Accumulated variation coefficient was assumed to be the same without time series change in grassland remaining grassland. Therefore, GHG removal of soil carbon was calculated as zero (0) in grassland remaining grassland.

    The grassland soil was sinks with constantly increasing of grassland area. But, land converted to grassland area constantly decreased and GHG removal of soil carbon was reduced. In 2012 (127.35 Gg CO2eq), this removal decreased 76% than in 1990 (535.71 Gg CO2eq). Total GHG removal in Korea were 50,937 Gg CO2eq in 2012. GHG removal of grassland sector was very small, accounted for 0.2% of the total (Ministry of the Environment, 2014). However, the study provides value by identifying grasslands as GHG sinks along with forests.

    IV.CONCLUSION

    This study provide GHG removal from 1990 to 2012 in grassland. This section divides grassland into two subcategories, “Grassland remaining Grassland” and “Land converted to Grassland”, and describes them separately in the following subsections. The grassland soil was sinks with constantly increasing of grassland area. GHG removal was reduced because land converted to grassland constantly decreased. But, GHG sinks are only grasslands and woodlands. It is important that grassland has been identified as a new GHG sinks with forests.

    Figure

    KGFS-35-251_F1.gif

    Grassland area with trend extrapolation.

    Table

    Default reference (under native vegetation) Soil Organic Carbon Stocks (SOCREF) (t C / ha, soil depth 0~30 cm)

    Grassland area from 1970 to 1977

    Grassland remaining grassland area by soil division

    Land converted to grassland area by soil division

    The greenhouse gas removal from 1990 to 2012 in grassland sector

    Reference

    1. Anderson JM (1991) The effects of climate change on decomposition processes in grassland and coniferous forests , Ecological Applications, Vol.1; pp.326-347
    2. Eswaran H , van den Berg E , Reich P (1993) Organic carbon in soils of the world , Soil science society of america journal, Vol.57; pp.192-194
    3. Intergovernmental Panel On Climate Change (2003) Good Practice Guidance for Land Use, Land-Use Change and Forestry , Institute for Global Environmental Strategies, pp.3.76
    4. Intergovernmental Panel On Climate (2003) Change Good PracticeGuidance for Land Use, Land-Use Change and Forestry , Institute for Global Environmental Strategies, pp.3.111
    5. Kang WG (2011) Soil classification and commentary in Korea , National academy of agricultural, pp.322-325
    6. Ministry of Land, Infrastructure and Transport (2013) Statistical yearbook of MOLIT,
    7. Ministry of the Environment, Japan (2015) National greenhouse gas inventory report of Japan , Greenhouse gas inventory office of Japan center for global enviromental research. Nation institute for environmetal studies, pp.6-1
    8. Ministry of the Environment, Korea (2014) National greenhouse gas inventory measuring, reporting and verification guidelines , Greenhouse gas inventory and research center of Korea, Vol.p; pp.73
    9. Ministry of the Environment, Korea (2014) National greenhouse gasinventory report of Korea , Greenhouse gas inventory and research center of korea, pp.243
    10. Post WM , Kwon KC (2000) Soil carbon sequestration andland-use change : processes and potential , Global Change Biology, Vol.6; pp.317-327