A LONG-TERM EFFECT OF N FERTILIZATION ON THE C-13 CPMAS NMR OF DE-ASHED SOIL HUMIN IN A 2ND-GROWTH DOUGLAS-FIR STAND OF COASTAL BRITISH-COLUMBIA

被引:67
作者
PRESTON, CM [1 ]
NEWMAN, RH [1 ]
机构
[1] IND RES LTD, GRACEFIELD RES CTR, LOWER HUTT, NEW ZEALAND
关键词
D O I
10.1016/0016-7061(95)00051-6
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Carbon-13 CPMAS NMR spectroscopy was used to examine long-term effects of thinning and N fertilization on the humin fraction of soil organic matter in a second-growth Douglas-fir stand of coastal British Columbia. De-ashed organic-matter-enriched humin fractions were prepared from three mineral soil horizons of four silvicultural treatments using 1.0 M HF accompanied by a magnetic stir bar to remove ferromagnetic iron particles, followed by a density separation. With some exceptions a higher proportion of mass was recovered in the denser, light-coloured fraction, and a higher proportion of C and N in the less-dense, dark fraction. In all cases, the less-dense fraction was enriched in total C compared to the original crude humin, and had a more favourable C/Fe ratio for NMR spectroscopy. The fraction of observable C was 33-37% for 8 of the samples, but as low as 7.6% for the remaining four. Carbon-13 CPMAS NMR spectra had typical features for humins (alkyl C, O-alkyl C, di-O-alkyl C, aromatic C, and carboxyl, ester and amide C). With fertilization, then was a small but consistent decrease in the ratio of alkyl to O-alkyl C, regardless of horizon or thinning, indicating a lower extent of decomposition. Carbon-13 subspectra based on proton spin relaxation time (T-1 (H-1)) were obtained for one fertilized and one unfertilized sample. Subspectra of the slowly-relaxing (long T-1(H-1)) domain were dominated by long-chain alkyl C. For the fertilized sample, the subspectrum of the fast-relaxing (short T-1(H-1)) domain had a higher proportion of O- and di-O-alkyl C, consistent with results from the normal CPMAS NMR spectra. Despite the uncertainties introduced by the de-ashing treatment and the low fraction of observable C, C-13 CPMAS NMR showed that fertilization has a long-term effect which is reflected in this humin fraction.
引用
收藏
页码:229 / 241
页数:13
相关论文
共 37 条
[1]  
Agriculture Canada Expert Committee on Soil Survey, 1987, AGR CAN PUBL, V1646
[2]   DEGRADATIVE STUDIES ON A SOIL HUMIN FRACTION - SEQUENTIAL DEGRADATION OF INHERITED HUMIN [J].
ALMENDROS, G ;
GONZALEZVILA, FJ .
SOIL BIOLOGY & BIOCHEMISTRY, 1987, 19 (05) :513-520
[3]   STRUCTURAL STUDY ON THE SOIL HUMIN FRACTION - BORON TRIFLUORIDE-METHANOL TRANSESTERIFICATION OF SOIL HUMIN PREPARATIONS [J].
ALMENDROS, G ;
SANZ, J .
SOIL BIOLOGY & BIOCHEMISTRY, 1991, 23 (12) :1147-1154
[4]   A STRUCTURAL STUDY OF ALKYL POLYMERS IN SOIL AFTER PERBORATE DEGRADATION OF HUMIN [J].
ALMENDROS, G ;
SANZ, J .
GEODERMA, 1992, 53 (1-2) :79-95
[5]   ATTEMPTS TO IMPROVE SOLID-STATE C-13 NMR-SPECTRA OF WHOLE MINERAL SOILS [J].
ARSHAD, MA ;
RIPMEESTER, JA ;
SCHNITZER, M .
CANADIAN JOURNAL OF SOIL SCIENCE, 1988, 68 (03) :593-602
[6]  
BALDOCK JA, 1992, BIOGEOCHEMISTRY, V16, P1, DOI 10.1007/BF02402261
[7]  
BALDOCK JA, 1995, CARBON FORMS AND FUNCTIONS IN FOREST SOILS, P89
[8]  
Bremner JM.., 1996, METHODS SOIL ANAL, P1085
[9]  
BRIX H, 1993, FERTILIZATION THINNI
[10]   FUNCTIONAL-GROUP CONTENT OF SOIL AND SEDIMENTARY HUMIC ACIDS DETERMINED BY CP/MAS C-13 NMR RELATED TO CONDITIONAL ZN2+ AND CD2+ FORMATION-CONSTANTS [J].
CAMERON, DF ;
SOHN, ML .
SCIENCE OF THE TOTAL ENVIRONMENT, 1992, 113 (1-2) :121-132