ESTIMASI CADANGAN KARBON PADA TANAH BEKAS TAMBANG EMAS DI KABUPATEN DHARMASRAYA, SUMATERA BARAT

Amsar Maulana, Mimien Harianti, T. Prasetyo, Herviyanti Herviyanti
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Abstract

Climate change, deforestation, and substantial loss of agricultural land within gold mining concessions in Dharmasraya greatly affect soil carbon stocks (Cs). This study used a survey method with purposive random sampling based on variations in ex-gold mining areas in each region, at depths of 0-20 and 20-40 cm with three to five replicates with a total of 54 samples. The estimation of Cs in ex-gold mining soil was highest at a depth of 20-40 cm (5.89E2), compared to a depth of 0-20 cm (1.38E2), where bulk density (BD), soil organic carbon (SOC), and total Hg in ex-gold mining soil at a depth of 0-20 and 20-40 cm were 1.46 and 1.39 g cm-3; 0.03 and 0.05%; 4.11 and 4.25 mg kg-1, respectively. The Cs in ex-gold mining soil at a depth of 0-20 cm is very significant by BD (r=-0.522** or Cs=-628.03(BD)+1055.1; R²=0.275) and SOC (r=0.948** or Cs=4896.8(SOC)-6.4673; R²=0.8996) and total Hg (r=0.518** or Cs=81.373(Hg)-196.43; R²=0.2688). However, at a depth of 20-40 cm, it was very significant by SOC (r=0.836** or Cs=16666(SOC)-196.03; R²=0.699).
气候变化、森林砍伐和在Dharmasraya金矿开采权范围内农业用地的大量流失极大地影响了土壤碳储量(Cs)。本研究采用有目的随机抽样的调查方法,根据各地区前金矿区的变化,在0 ~ 20 cm和20 ~ 40 cm深度进行调查,共3 ~ 5次重复,共54份样本。前金矿土壤Cs在20 ~ 40 cm (5.89E2)处估计值最高,0 ~ 20 cm (1.38E2)处估计值最高,0 ~ 20 cm和20 ~ 40 cm的容重(BD)、土壤有机碳(SOC)和总汞(Hg)分别为1.46和1.39 g cm-3;0.03和0.05%;分别为4.11和4.25 mg kg-1。在0 ~ 20 cm深度前金矿土壤中,Cs具有显著的BD值(r=-0.522**或Cs=-628.03(BD)+1055.1);R²=0.275)和SOC (R =0.948**或Cs=4896.8(SOC)-6.4673;R²=0.8996)和总汞(R =0.518**或Cs=81.373(Hg)-196.43);R²= 0.2688)。而在20 ~ 40 cm深度,SOC (r=0.836**或Cs=16666(SOC)-196.03)非常显著;R²= 0.699)。
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