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

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)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ESTIMASI CADANGAN KARBON PADA TANAH BEKAS TAMBANG EMAS DI KABUPATEN DHARMASRAYA, SUMATERA BARAT
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).
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