کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
6308406 1618854 2014 7 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Calculating carbon mass balance from unsaturated soil columns treated with CaSO4-minerals: Test of soil carbon sequestration
موضوعات مرتبط
علوم زیستی و بیوفناوری علوم محیط زیست شیمی زیست محیطی
پیش نمایش صفحه اول مقاله
Calculating carbon mass balance from unsaturated soil columns treated with CaSO4-minerals: Test of soil carbon sequestration
چکیده انگلیسی


- Soil carbon mass balance was calculated in an unsaturated soil column.
- Soil amendment with CaSO4-minerals works for carbon sequestration.
- Main carbon sequestration resulted from organic carbon retention.
- Precipitated calcite can be considered as a carbon sink in this study.
- CaSO4-soil amendment is proved as a effective carbon sequestration method.

Renewed interest in managing C balance in soils is motivated by increasing atmospheric concentrations of CO2 and consequent climate change. Here, experiments were conducted in soil columns to determine C mass balances with and without addition of CaSO4-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 CO2 to the atmosphere rather than from chemical leaching. Microbial oxidation of SOC appears to have been suppressed by increased Ca2+ and SO42− from dissolution of CaSO4 minerals. For the conditions tested, SIC accumulation per m2 soil area under CaSO4-treatment ranged from 130 to 260 g C m−1 infiltrated water (20-120 g C m−1 infiltrated water as net C benefit). These results demonstrate the potential for increasing C sequestration in slightly alkaline soils via CaSO4-treatment.

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ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Chemosphere - Volume 117, December 2014, Pages 87-93
نویسندگان
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