Interactive effects of tillage system and soil water content on aggregate size distribution for seedbed preparation in Fluvisols in southwest Iran

被引:37
作者
Barzegar, AR [1 ]
Hashemi, AM
Herbert, SJ
Asoodar, MA
机构
[1] Univ Massachusetts, Dept Plant & Soil Sci, Amherst, MA 01003 USA
[2] Shahid Chamran Univ, Dept Soil Sci, Coll Agr, Ahvaz, Iran
[3] Shahid Chamran Univ, Dept Agr Machinery, Ramin Agr Res & Educ Sch, Ahvaz, Iran
关键词
aggregate size distribution; soil water content; tillage; Iran;
D O I
10.1016/j.still.2004.01.002
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
A proper aggregate size distribution is an important factor in successful crop production in semi-arid region. Field experiments were conducted on both silty clay loam and loam soils (Calcaric Fluvisols, FAO) in semi-arid area of southwest of Iran to assess the effect of different tillage systems and soil water contents on aggregate size distribution in plowed layers (250 mm depth). Three tillage treatments, moldboard plowing followed by disc harrowing (MD); disc plowing using disc plow followed by disc harrowing (DD); disking using offset disc followed by disc harrowing (OD) were used. Each tillage treatment was implemented at four soil water contents, viz. 0.8, 0.7, 0.6 and 0.5w(PL) (plastic limit). The aggregate size distributions for each tillage-soil water content were determined of 0-50, 50-100, 100-150 and 150-250 mm soil layers. Tillage systems and soil water contents both showed significant effects on aggregate size distribution. In silty clay loam soil, the greatest proportion of <5 mm and the lowest proportions of >25 mm aggregates were obtained by MD and DD tillage treatments at 0.8w(PL), and for OD at 0.7w(PL). The percentage of <5 mm aggregates for MD, DD and OD tillage treatments for the aforementioned water contents were ranged 42-47, 33-35 and 22-45%, respectively. However, for loam soil, the greatest proportion of <5 mm and the lowest proportions of >25 mm aggregates were obtained by MD and DD tillage treatments at 0.7w(PL), and for OD at 0.8w(PL). The percentage of <5 mm aggregates for MD, DD and OD tillage treatments for the aforementioned water content were ranged 40-49, 22-47 and 37-51 %, respectively. Results indicated that aggregate size distribution of plowed layers under various tillage systems vary with soil water content and soil type. (C) 2004 Elsevier B.V. All rights reserved.
引用
收藏
页码:45 / 52
页数:8
相关论文
共 22 条
[1]  
[Anonymous], 1975, 1377 BRIT STAND I
[2]   Soil structure degradation and mellowing of compacted soils by saline sodic solutions [J].
Barzegar, AR ;
Oades, JM ;
Rengasamy, P .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1996, 60 (02) :583-588
[3]   EFFECTS OF CLAY TYPE AND RATE OF WETTING ON THE MELLOWING OF COMPACTED SOILS [J].
BARZEGAR, AR ;
RENGASAMY, P ;
OADES, JM .
GEODERMA, 1995, 68 (1-2) :39-49
[4]   SOIL AGGREGATION IN THE SEEDBED - A REVIEW .2. EFFECT OF AGGREGATE SIZES ON PLANT-GROWTH [J].
BRAUNACK, MV ;
DEXTER, AR .
SOIL & TILLAGE RESEARCH, 1989, 14 (03) :281-298
[5]   Effect of soil macroporosity and aggregate size on seed-soil contact [J].
Brown, AD ;
Dexter, AR ;
Chamen, WCT ;
Spoor, G .
SOIL & TILLAGE RESEARCH, 1996, 38 (3-4) :203-216
[6]   Methods for predicting the optimum and the range of soil water contents for tillage based on the water retention curve [J].
Dexter, AR ;
Bird, NRA .
SOIL & TILLAGE RESEARCH, 2001, 57 (04) :203-212
[7]   Emergence of seedlings of sugar beet (Beta vulgaris L.) as affected by the size, roughness and position of aggregates in the seedbed [J].
Dürr, C ;
Aubertot, JN .
PLANT AND SOIL, 2000, 219 (1-2) :211-220
[8]  
Gee G.W., 2002, METHODS SOIL ANAL, P255, DOI DOI 10.2136/SSSABOOKSER5.1.2ED.C15
[9]   A review of tillage effects on crop residue management, seedbed conditions and seedling establishment [J].
Guérif, J ;
Richard, G ;
Dürr, C ;
Machet, JM ;
Recous, S ;
Roger-Estrade, J .
SOIL & TILLAGE RESEARCH, 2001, 61 (1-2) :13-32
[10]   A review of research on seedbed preparation for small grains in Sweden [J].
Håkansson, I ;
Myrbeck, Å ;
Etana, A .
SOIL & TILLAGE RESEARCH, 2002, 64 (1-2) :23-40