RISS 학술연구정보서비스

검색
다국어 입력

http://chineseinput.net/에서 pinyin(병음)방식으로 중국어를 변환할 수 있습니다.

변환된 중국어를 복사하여 사용하시면 됩니다.

예시)
  • 中文 을 입력하시려면 zhongwen을 입력하시고 space를누르시면됩니다.
  • 北京 을 입력하시려면 beijing을 입력하시고 space를 누르시면 됩니다.
닫기
    인기검색어 순위 펼치기

    RISS 인기검색어

      SCOPUS SCIE

      Calculating carbon mass balance from unsaturated soil columns treated with CaSO<sub>4</sub>-minerals: Test of soil carbon sequestration

      한글로보기

      https://www.riss.kr/link?id=A107542087

      • 0

        상세조회
      • 0

        다운로드
      서지정보 열기
      • 내보내기
      • 내책장담기
      • 공유하기
      • 오류접수

      부가정보

      다국어 초록 (Multilingual Abstract)

      <P><B>Abstract</B></P> <P>Renewed interest in managing C balance in soils is motivated by increasing atmospheric concentrations of CO<SUB>2</SUB> and consequent climate change. Here, experiments were conducte...

      <P><B>Abstract</B></P> <P>Renewed interest in managing C balance in soils is motivated by increasing atmospheric concentrations of CO<SUB>2</SUB> and consequent climate change. Here, experiments were conducted in soil columns to determine C mass balances with and without addition of CaSO<SUB>4</SUB>-minerals (anhydrite and gypsum), which were hypothesized to promote soil organic carbon (SOC) retention and soil inorganic carbon (SIC) precipitation as calcite under slightly alkaline conditions. Changes in C contents in three phases (gas, liquid and solid) were measured in unsaturated soil columns tested for one year and comprehensive C mass balances were determined. The tested soil columns had no C inputs, and only C utilization by microbial activity and C transformations were assumed in the C chemistry. The measurements showed that changes in C inventories occurred through two processes, SOC loss and SIC gain. However, the measured SOC losses in the treated columns were lower than their corresponding control columns, indicating that the amendments promoted SOC retention. The SOC losses resulted mostly from microbial respiration and loss of CO<SUB>2</SUB> to the atmosphere rather than from chemical leaching. Microbial oxidation of SOC appears to have been suppressed by increased Ca<SUP>2+</SUP> and SO<SUB>4</SUB> <SUP>2</SUP> <SUP>−</SUP> from dissolution of CaSO<SUB>4</SUB> minerals. For the conditions tested, SIC accumulation per m<SUP>2</SUP> soil area under CaSO<SUB>4</SUB>-treatment ranged from 130 to 260gCm<SUP>−1</SUP> infiltrated water (20–120gCm<SUP>−1</SUP> infiltrated water as net C benefit). These results demonstrate the potential for increasing C sequestration in slightly alkaline soils via CaSO<SUB>4</SUB>-treatment.</P> <P><B>Highlights</B></P> <P> <UL> <LI> Soil carbon mass balance was calculated in an unsaturated soil column. </LI> <LI> Soil amendment with CaSO<SUB>4</SUB>-minerals works for carbon sequestration. </LI> <LI> Main carbon sequestration resulted from organic carbon retention. </LI> <LI> Precipitated calcite can be considered as a carbon sink in this study. </LI> <LI> CaSO<SUB>4</SUB>-soil amendment is proved as a effective carbon sequestration method. </LI> </UL> </P> <P><B>Graphical abstract</B></P> <P>[DISPLAY OMISSION]</P>

      더보기

      분석정보

      View

      상세정보조회

      0

      Usage

      원문다운로드

      0

      대출신청

      0

      복사신청

      0

      EDDS신청

      0

      동일 주제 내 활용도 TOP

      더보기

      주제

      연도별 연구동향

      연도별 활용동향

      연관논문

      연구자 네트워크맵

      공동연구자 (7)

      유사연구자 (20) 활용도상위20명

      이 자료와 함께 이용한 RISS 자료

      나만을 위한 추천자료

      해외이동버튼