减少罗马尼亚一些栽培矿质土壤的温室气体排放

O. Vizitiu, I. Calciu
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摘要

管理措施的影响导致了农业土壤净碳平衡的显著变化,本文估算了长期耕作对土壤有机碳储量的影响。本文还评估了在干燥气候条件下,通过温带农业系统管理实践对矿质土壤固碳的潜力。为实现本研究的目的,采用-储量差法-估算t1(2000)和t2(2021)两个时间点之间的土壤有机碳储量。结果表明:2000 ~ 2021年21年间,大部分土壤有机碳储量的变化均呈现出显著的增加趋势,但有一个例外,土壤有机碳储量减少了约50%。11%记录在案。Cambic黑钙土的有机碳储量增幅最大,与2000年相比,2021年的有机碳储量增加了63%。土壤碳储量年变化率最高(1.4762 tC/ha),其次是黑钙土(1.4286 tC/ha)、黑钙土(1.3810 tC/ha)和氟维松土(1.0476 tC/ha)。结果表明,寒武系黑钙岩对大气CO2的去除潜力最大,年去除速率为5.41 tCO2/ha。富营养化Cambisol和黑钙土具有较高的CO2固存潜力,累积速率分别为5.24 tCO2/ha和5.06 tCO2/ha。
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MITIGATION OF GREENHOUSE GAS EMISSIONS IN SOME CULTIVATED MINERAL SOILS FROM ROMANIA
The effect of management practices lead to significant variations of the net C balance of agricultural soils, and in this paper is estimated the impact of long-term cultivation on the soil organic carbon stocks. This paper also evaluates the potential of carbon sequestration of mineral soils through management practices in temperate agricultural systems, under dry climate regime. For fulfilling of the objective of this study, the -stock-difference method- was used for estimating the soil organic carbon stocks between two points in time, t1 (2000) and t2 (2021). The results obtained showed that the evolution of SOC stocks during the 21 years period between 2000 and 2021 recorded significant increases in most of the investigated soils, with one exception where a decrease in SOC stock by aprox. 11 % was recorded. The highest increase in SOC stock was recorded in case of a Cambic Chernozem soil, where the SOC stock value from 2021 is 63% higher as compared with the SOC value from 2000. Also, this soil recorded the highest rate for annual change in carbon stock (1.4762 tC/ha), followed by Eutric Cambisol (1.4286 tC/ha), Chernozem (1.3810 tC/ha) and Fluvisol (1.0476 tC/ha). The presented results showed that the Cambic Chernozem has the highest potential for CO2 removal from the atmosphere with an annual rate of 5.41 tCO2/ha. Also, high potentials for CO2 sequestration with accumulation rates of 5.24 tCO2/ha and respectively 5.06 tCO2/ha have the Eutric Cambisol and Chernozem soils.
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