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shook two ways to estimate reserves are mainly libraries, one library net flux multiplied by the residence time, the second is the library of organic carbon stock multiplied by the black carbon concentration. Table
3 shows that reserves of soil, air, marine and other three black carbon stocks is relatively consistent in both estimation method, and a larger difference between the two estimates of sediment reserves. Shake Table 3 estimates of black carbon main Storage in Table 3 Shake Estimation of major pools of black carbon estimation method a Method A library library organic Estimation Method Two Method B black carbon concentration reserves of Pools library net flux / (Tg / a) Net flux retention time / A Residence time library reserves / PGA Reserve, carbon storage / Pg Organic carbon Reserve / (the BC / the TOC) Black carbon Concentration / Pg Reserve, soil soil 20 -200 500 -5000 [86] 10 -1000 1580 [1] % -40% 10 [86] 160 -600 7000 [66] 350 -1 900 [66] 0 14 -0. 4 a Tg of 5. 1 108 * Ina 0.31 by 0.10 [89] ** (0. by 16 0. 05) a Tg of 25 [83] 10% [86] 2. 5 <140. 700 [1] 4% -22% [83] 28 -154 90 -180 150 [1] 20% [1] 30 the Surface sediment 1 (open sea) 10000-20000 [86] 10-20 sediment sediment 30000 [88] (offshore) 5% -38% [68] -10000 1500 set to 1500 [66] (open sea) of 12% -31% [83] 180-450
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