Soil carbon and nitrogen changes as influenced by tillage and cropping systems in some Iowa soils

被引:211
作者
Al-Kaisi, MM [1 ]
Yin, XH [1 ]
Licht, MA [1 ]
机构
[1] Iowa State Univ, Dept Agron, Ames, IA 50011 USA
关键词
cropping system; smooth bromegrass; soil organic carbon; switchgrass; tillage; total nitrogen;
D O I
10.1016/j.agee.2004.08.002
中图分类号
S [农业科学];
学科分类号
09 ;
摘要
Soil organic C (SOC) and total N (TN) contents play a crucial role in sustaining agricultural production systems. Short-term (<= 10-year) management effects on SOC and TN dynamics are often complex and variable. Three experiments were conducted to evaluate short-term tillage and cropping system effects on SOC and TN within the 0-30 cm soil depth across Iowa. The first experiment with no-tillage and chisel plowing treatments was established in 1994 on Clarion-Nicollet-Webster (CNW), Galva-Primghar-Sac (GPS), Kenyon-Floyd-Clyde (KFC), Marshall (M), and Otley-Mahaska-Taintor (OMT) soil associations under a corn (Zea mays L.)-soybean (Glycine max (L.) Merr.) rotation. The second experiment with no-tillage, strip-tillage, chisel plowing, deep ripping, and moldboard plowing treatments was initiated in 1998 on the CNW soil association in a corn-soybean rotation. The third experiment consisting of smooth bromegrass (Bromus inermis Leyss.), switchgrass (Panicum virgatum L.) and com-soybean-alfalfa (Medicago sativa L.) treatments was established in 1991 on Monona-Ida-Hamburg (MIH) soil association under no-tillage management. Short-term tillage effects on SOC and TN occurred primarily at the 0-15 cm soil depth. Tillage effects did not vary significantly with soil association. No-tillage resulted in greater SOC and TN contents than chisel plowing at the end of 7 years of tillage practices averaged over the CNW, GPS, KFC, M, and OMT soil associations. The increase in SOC and TN with no-tillage was not related to SOC and TN stratification in the soil profile or annual C and N inputs from crop residue, but most likely due to decreased mineralization rate of soil organic matter. However, tillage effects on SOC and TN were negligible at the end of only 3 years of tillage practices on the CNW soil association. Smooth bromegrass and switchgrass systems resulted in greater SOC and TN contents at both 0-15 cm and 15-30 cm soil depths than a com-soybean-alfalfa rotation after 10 years of management on the MIH soil association. Smooth bromegrass and switchgrass systems increased SOC by 2.3 and 1.2 Mg ha(-1) yr(-1) at the 0-15 cm soil depth, respectively. We conclude from these short-term experiments that reducing tillage intensity and increasing crop diversity to include perennial grasses could be effective in improving C and N sequestration in Midwest soils. (c) 2004 Elsevier B.V All rights reserved.
引用
收藏
页码:635 / 647
页数:13
相关论文
共 42 条
[21]   CROP-ROTATION AND TILLAGE EFFECTS ON SOIL ORGANIC-CARBON AND NITROGEN [J].
HAVLIN, JL ;
KISSEL, DE ;
MADDUX, LD ;
CLAASSEN, MM ;
LONG, JH .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1990, 54 (02) :448-452
[22]   A SIMPLE METHOD FOR CALCULATING DECOMPOSITION AND ACCUMULATION OF YOUNG SOIL ORGANIC-MATTER [J].
JANSSEN, BH .
PLANT AND SOIL, 1984, 76 (1-3) :297-304
[23]   EFFECT OF MOISTURE-CONTENT, TEMPERATURE AND NITROGEN-FERTILIZATION ON CARBON-DIOXIDE EVOLUTION FROM FIELD SOILS [J].
KOWALENKO, CG ;
IVARSON, KC ;
CAMERON, DR .
SOIL BIOLOGY & BIOCHEMISTRY, 1978, 10 (05) :417-423
[24]  
Lal R., 1998, POTENTIAL US CROPLAN
[25]  
LAL R, 1995, ADV SOIL SCI SOIL MA
[26]  
LICHT MA, 2003, THESIS LIB IOWA STAT
[27]   MODELING SOIL ORGANIC-MATTER IN ORGANIC-AMENDED AND NITROGEN-FERTILIZED LONG-TERM PLOTS [J].
PAUSTIAN, K ;
PARTON, WJ ;
PERSSON, J .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1992, 56 (02) :476-488
[28]   Management options for reducing CO2 emissions from agricultural soils [J].
Paustian, K ;
Six, J ;
Elliott, ET ;
Hunt, HW .
BIOGEOCHEMISTRY, 2000, 48 (01) :147-163
[29]  
REICOSKY DC, 1995, J SOIL WATER CONSERV, V50, P253
[30]   Tillage-induced CO2 emission from soil [J].
Reicosky, DC .
NUTRIENT CYCLING IN AGROECOSYSTEMS, 1997, 49 (1-3) :273-285