Charcoal effects on soil solution chemistry and growth of Koeleria macrantha in the ponderosa pine/Douglas-fir ecosystem

被引:173
作者
Gundale, Michael J. [1 ]
DeLuca, Thomas H. [1 ]
机构
[1] Univ Montana, Dept Ecosyst & Conservat Sci, Missoula, MT 59812 USA
关键词
charcoal; soil solution chemistry; Douglas-fir and ponderosa pine ecosystems;
D O I
10.1007/s00374-006-0106-5
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
We conducted laboratory and greenhouse experiments to determine whether charcoal derived from the ponderosa pine/Douglas-fir ecosystem may influence soil solution chemistry and growth of Koeleria macrantha, a perennial grass that thrives after fire. In our first experiment, we incubated forest soils with a factorial combination of Douglas-fir wood charcoal generated at 350 degrees C and extracts of Arctostaphylos uva-ursi with and without the addition of glycine as a labile N source. These results showed that charcoal increased N mineralization and nitrification when glycine was added, but reduced N mineralization and nitrification without the addition of glycine. Charcoal significantly reduced the solution concentration of soluble phenols from litter extracts, but may have contributed bioavailable C to the soil that resulted in N immobilization in the no-glycine trial. In our second experiment, we grew K. macrantha in soil amended with charcoal made at 350 degrees C from ponderosa pine and Douglas-fir bark. Growth of K. macrantha was significantly diminished by both of these charcoal types relative to the control. In our third experiment, we grew K. macrantha in soil amended with six concentrations (0, 0.5, 1, 2, 5, and 10%) of charcoal collected from a wildfire. The data showed increasing growth of K. macrantha with charcoal addition, suggesting some fundamental differences between laboratory-generated charcoal and wildfire-produced charcoal. Furthermore, they suggest a need for a better understanding of how temperature and substrate influence the chemical properties of charcoal.
引用
收藏
页码:303 / 311
页数:9
相关论文
共 37 条
[1]   Activated carbon amendments to soil alters nitrification rates in Scots pine forests [J].
Berglund, LM ;
DeLuca, TH ;
Zackrisson, O .
SOIL BIOLOGY & BIOCHEMISTRY, 2004, 36 (12) :2067-2073
[2]  
Covington W.W., 1990, RM191 USDA FOR SERV, P105
[3]   SOIL MINERAL NITROGEN CHANGES FOLLOWING PRESCRIBED BURNING IN PONDEROSA PINE [J].
COVINGTON, WW ;
SACKETT, SS .
FOREST ECOLOGY AND MANAGEMENT, 1992, 54 (1-4) :175-191
[4]   EFFECTS OF BURNING ON CHAPARRAL SOILS .1. SOIL-NITROGEN [J].
DEBANO, LF ;
EBERLEIN, GE ;
DUNN, PH .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1979, 43 (03) :504-509
[5]   Nitrogen mineralization and phenol accumulation along a fire chronosequence in northern Sweden [J].
DeLuca, TH ;
Nilsson, MC ;
Zackrisson, O .
OECOLOGIA, 2002, 133 (02) :206-214
[6]   Wildfire-produced charcoal directly influences nitrogen cycling in ponderosa pine forests [J].
DeLuca, TH ;
MacKenzie, MD ;
Gundale, MJ ;
Holben, WE .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 2006, 70 (02) :448-453
[7]   Effects of selection harvest and prescribed fire on the soil nitrogen status of ponderosa pine forests [J].
DeLuca, TH ;
Zouhar, KL .
FOREST ECOLOGY AND MANAGEMENT, 2000, 138 (1-3) :263-271
[8]   Bacterial activity in a forest soil after soil heating and organic amendments measured by the thymidine and leucine incorporation techniques [J].
DiazRavina, M ;
Prieto, A ;
Baath, E .
SOIL BIOLOGY & BIOCHEMISTRY, 1996, 28 (03) :419-426
[9]   EFFECTS OF BURNING ON CHAPARRAL SOILS .2. SOIL MICROBES AND NITROGEN MINERALIZATION [J].
DUNN, PH ;
DEBANO, LF ;
EBERLEIN, GE .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1979, 43 (03) :509-514
[10]   Organic matter changes immediately after a wildfire in an Atlantic forest soil and comparison with laboratory soil heating [J].
Fernandez, I ;
Cabaneiro, A ;
Carballas, T .
SOIL BIOLOGY & BIOCHEMISTRY, 1997, 29 (01) :1-11