Estimating soil organic carbon through loss on ignition: effects of ignition conditions and structural water loss

被引:299
作者
Hoogsteen, M. J. J. [1 ]
Lantinga, E. A. [1 ]
Bakker, E. J. [2 ]
Groot, J. C. J. [1 ]
Tittonell, P. A. [1 ]
机构
[1] Univ Wageningen & Res Ctr, Dept Plant Sci, Farming Syst Ecol Grp, NL-6708 PB Wageningen, Netherlands
[2] Univ Wageningen & Res Ctr, Dept Plant Sci, Math & Stat Methods, NL-6708 PB Wageningen, Netherlands
关键词
LOSS-ON-IGNITION; MATTER;
D O I
10.1111/ejss.12224
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Loss on ignition (LOI) is one of the most widely used methods for measuring organic matter content in soils but does not have a universal standard protocol. A large number of factors may influence its accuracy, such as furnace type, sample mass, duration and temperature of ignition and clay content of samples. We conducted a series of experiments to quantify these effects, which enabled us to derive (i) guidelines for ignition conditions (sample mass, duration and temperature), (ii) temperature-specific soil organic matter (SOM) to soil organic carbon (SOC) conversion factors and (iii) clay content-dependent correction factors for structural water loss (SWL). Bulk samples of a sandy soil (4% clay) and a silt loam soil (25% clay) were used to evaluate the effects of ignition conditions. Samples with a range of clay contents (0-50%) were used to quantify conversion and correction factors. Two furnaces, one without and one with pre-heated air, did not show significant differences in terms of within-batch LOI variability. In both furnaces less combustion occurred close to the door, which necessitated tray turning at half-time as this reduced the standard deviation per batch significantly. Variation in mass loss declined exponentially with sample mass (range, 0.15-20g). The LOI increased with duration at lower temperatures (550 degrees C) for the sandy soil. At greater temperatures (600 and 650 degrees C), no effect of duration was found. For the silt loam soil, LOI values increased with duration for each temperature, which was attributed to SWL. The SOM to SOC conversion factor decreased strongly with temperature at an ignition duration of 3hours from 0.70 (350 degrees C) to 0.57 (500 degrees C) and stabilized around 0.55 between 550 and 650 degrees C, indicating that at temperatures 550 degrees C all SOM had been removed. The clay correction factor for SWL increased from 0.01 to 0.09 as the temperature of ignition increased from 350 to 650 degrees C. To minimize within-batch LOI variation we recommend a standard ignition duration of 3hours, tray turning at half-time, a sample mass 20g and temperatures equal to or greater than 550 degrees C. To avoid over-estimates of SOM through structural water loss, the presented SWL correction procedure should always be applied.
引用
收藏
页码:320 / 328
页数:9
相关论文
共 32 条
[1]   Estimating organic carbon from loss-on-ignition in northern Arizona forest soils [J].
Abella, Scott R. ;
Zimmer, Brian W. .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 2007, 71 (02) :545-550
[2]   LOSS-ON-IGNITION AS ESTIMATE OF ORGANIC MATTER + ORGANIC CARBON IN NON-CALCAREOUS SOILS [J].
BALL, DF .
JOURNAL OF SOIL SCIENCE, 1964, 15 (01) :84-&
[3]  
Breeuwsma A., 1987, Bodemkunde van Nederland eds, P95
[4]  
Buringh P., 1951, THESIS LANDBOUWHOGES, P57
[5]  
CARVER RE, 1981, J SEDIMENT PETROL, V51, P658
[6]  
CHRISTENSEN BT, 1982, HOLARCTIC ECOL, V5, P376
[7]   LOSS-ON-IGNITION AS AN ESTIMATE OF SOIL ORGANIC-MATTER [J].
DAVIES, BE .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1974, 38 (01) :150-151
[8]   Capability of loss-on-ignition as a predictor of total organic carbon in non-calcareous forest soils [J].
De Vos, B ;
Vandecasteele, B ;
Deckers, J ;
Muys, B .
COMMUNICATIONS IN SOIL SCIENCE AND PLANT ANALYSIS, 2005, 36 (19-20) :2899-2921
[9]   Comparison of theories for the variance caused by the sampling of random mixtures of non-identical particles [J].
Geelhoed, B ;
Glass, HJ .
GEOSTANDARDS AND GEOANALYTICAL RESEARCH, 2004, 28 (02) :263-276
[10]   A COMPARISON OF 3 METHODS OF ORGANIC-CARBON DETERMINATION IN SOME NEW-ZEALAND SOILS [J].
GREWAL, KS ;
BUCHAN, GD ;
SHERLOCK, RR .
JOURNAL OF SOIL SCIENCE, 1991, 42 (02) :251-257