GEOCHEMICAL FEATURES OF POST-PYROGENIC CHANGES OF POLISSYA SOILS (LOW FIRE)

IF 0.5 Q4 MINERALOGY Mineralogical Journal-Ukraine Pub Date : 2021-01-01 DOI:10.15407/mineraljournal.43.03.091
N. Kryuchenko, E. Zhovinsky, P.S. Paparуga
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Abstract

Geochemical post-pyrogenic soil changes are one of the most important factors in determining the state of the forest ecosystem. For the first time the content of microelements (Hg, As, Ba, Mg, Mn, Mo, Cd, Co, Cr, Cu, Pb, Zn, V, Ni) in post-pyrogenic sod-podzolic soils under the pine forest of Zhytomyr Polissya (Ukraine) was determined by the ICP-MS method. The study is based on a comparison of the content of trace elements in the sod-podzolic soils of the background area and burnt areas (grassland fire in 2019). The analysis of microelements in the soil profile of the burned and background areas to a depth of 10 cm (after 1 cm) and set the limit - 3-5 cm (humus-eluvial horizon), after which you can record the accumulation or scattering of elements after a fire on the surface. By calculating the percentage change (relative to background soils), intensive accumulation (more than 20%) of elements in post-pyrogenic soils - Cu, Ni, Co, V and moderate accumulation (up to 10%) - Pb, Mo, Mg, Ba, Cr and intensive scattering - Hg, As, Cd, Zn, Mn. The increase in the pH of post-pyrogenic soils (from 4.2 to 7.5) was determined, spatial map-schemes were constructed, due to which the direction of the fire was revealed - from the south-east to the north-west. The change of the content of ionic forms of metals (Cu, Pb, Zn, Mn) in the soil solution at different pH values (from 4 to 8 with a step of 0.2) is modeled (PHREEQC program) and the current trend is revealed: Pb - linear dependence, Cu, Zn, Mn is polynomial. The pH limits are calculated, where there are free forms of metals that enter the plants: Pb 3.9-8.2; Zn 5.5-7.5; Cu 5-8.2; Mn 5-11.5. The post-fire transformation of soils was revealed, which is expressed in the increase of pH (before the fire - 4.2-4.8; after the fire - 6.5-7.2; a year after the fire - 4.5-5.5). The obtained results confirmed the need for geochemical monitoring of post-pyrogenic soils for ecosystem restoration and plant biodiversity.
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polissya土壤(低火)热生后变化的地球化学特征
热生后土壤地球化学变化是决定森林生态系统状态的重要因素之一。首次采用ICP-MS法测定了乌克兰Zhytomyr Polissya松林下热原后草灰化土壤中微量元素Hg、As、Ba、Mg、Mn、Mo、Cd、Co、Cr、Cu、Pb、Zn、V、Ni的含量。该研究是基于对背景区和烧毁区(2019年草原火灾)草灰土壤中微量元素含量的比较。在燃烧和背景区域的土壤剖面中分析微量元素,深度为10厘米(后1厘米),并设定限制- 3-5厘米(腐殖质-残积层),之后可以记录元素在火灾后在表面的积累或散射。通过计算变化百分比(相对于背景土壤),发现热原后土壤中Cu、Ni、Co、V元素的富集(超过20%)和Pb、Mo、Mg、Ba、Cr元素的富集(高达10%)和Hg、As、Cd、Zn、Mn元素的富集(高达10%)。确定了热原后土壤pH值的增加(从4.2到7.5),构建了空间地图方案,由此揭示了火灾的方向-从东南到西北。利用PHREEQC程序模拟了不同pH值(4 ~ 8,步长为0.2)下土壤溶液中金属(Cu、Pb、Zn、Mn)离子形态含量的变化,揭示了其变化趋势:Pb呈线性关系,Cu、Zn、Mn呈多项式关系。计算了进入植物的自由形式金属的pH极限:Pb 3.9-8.2;锌5.5 - -7.5;铜5 - 8.2;Mn 5 - 11.5。结果表明,火灾发生后土壤的变化表现为pH值升高(火灾前- 4.2 ~ 4.8;后火- 6.5-7.2;火灾后一年(4.5-5.5)。研究结果证实了对热原后土壤进行地球化学监测对生态系统恢复和植物多样性的必要性。
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CiteScore
0.70
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0.00%
发文量
18
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