16 Mayer L M. The inertness of being organic. Mar Chem, 2004, 92: 135-140
[2]
17 Skiba M, Szczerba M, Skiba S, et al. The nature of interlayering in clays from a podzol (Spodosol) from the Tatra Mountains, Poland. Geoderma, 2011,160: 425-433
27 Ransom B, Kim D, Kastner M, et al. Organic matter preservation on continental slopes: Importance of mineralogy and surface area. Geochim Cosmochim Acta, 1998, 62: 1329-1345
29 Oladipo E O, Randy J M. High surface areas caused by smectitic interstratification of kaolinite and illite in Athabasca oil sands. Appl Clay Sci, 2004, 25: 37-47
32 Schulten H R, Leinweber P, Theng B K G. Characterization of organic matter in an interlayer clay-organic complex from soil by pyrolysis methylation-mass spectrometry. Geoderma, 1996, 69: 105-118
[13]
1 Mayer L M. Surface area control on organic carbon accumulation in continental shelf sediments. Geochim Cosmochim Acta, 1994, 58: 1271-1284
[14]
2 Mayer L M, Xing B S. Organic matter-surface area relationships in acid soils. Soil Sci Soc Am J, 2001, 65: 250-258
[15]
3 Mayer L M, Schick L L, Hardy K R, et al. Organic matter in small mesopores in sediments and soils. Geochim Cosmochim Acta, 2004, 68: 3863-3872
[16]
4 Kennedy M, Droser M, Mayer L M, et al. Late precambrian oxygenation; inception of the clay mineral factory. Science, 2006, 311: 1446-1449
[17]
5 Ralph N M, Miguel A G. Matrix protected organic matter in a river dominated margin: A possible mechanism to sequester terrestrial organic matter? Geochim Cosmochim Acta, 2008, 72: 2673-2686
[18]
6 Mikutta R, Schaumann G E, Gildemeister D, et al. Biogeochemistry of mineral-organic associations across a long-term mineralogical soil gradient (0.3-4100 kyr), Hawaiian Islands. Geochim Cosmochim Acta, 2009, 73: 2034-2060
[19]
7 Tosca N J, Johnston D T, Mushegian A, et al. Clay mineralogy, organic carbon burial, and redox evolution in Proterozoic oceans. Geochim Cosmochim Acta, 2010, 74: 1579-1592
[20]
8 Bruun T B, Elberling B, Christensen B T. Lability of soil organic carbon in tropical soils with different clay minerals. Soil Boil Biochem, 2010, 42: 888-895
[21]
9 Clemente J S, Simpson A J, Simpson M J. Association of specific organic matter compounds in size fractions of soils under different environmental controls. Org Geochem, 2011, 42: 1169-1180
[22]
10 Kennedy M J, Pevear D R, Hill R J. Mineral surface control of organic carbon in black shale. Science, 2002, 295: 657-660
12 Arnarson T S, Keil R G. Changes in organic matter-mineral interactions for marine sediments with varying oxygen times. Geochim Cosmochim Acta, 2007, 71: 3545-3356
[25]
13 Sollins P, Hofmann P, Caldweel B A. Stabilization and destabilization of soil organic matter: Mechanism and controls. Geoderma, 1996, 74: 65-105
[26]
14 Baldock J A, Skjemstad T O. Role of soil matrix and minerals in protecting natural organic materials against biological attack. Org Geochem, 2000, 31: 697-710
[27]
15 Six J, Conant R T, Paul E A. Stabilization mechanisms of soil organic matter: implications for C-saturation of soil. Plant Soil, 2002, 241: 155-176
24 Bartoli F, Poulenard A J, Schouller B E. Influence of allophane and organic matter contents on surface properties of Andosols. Eur J Soil Sci, 2007, 58: 450-464
