TILLAGE MANAGEMENT CHANGES SIZE-DISTRIBUTION OF AGGREGATES AND MACRO-STRUCTURE OF SOILS USED FOR IRRIGATED ROW-CROPS

被引:32
作者
ADEM, HH
TISDALL, JM
WILLOUGHBY, P
机构
关键词
D O I
10.1016/0167-1987(84)90005-9
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The Tatura system for the preparation of seed-beds for irrigated annual row-crops is described, where the soil is tilled when wet and friable and so requires few passes with implements to become suitable for crops, and where seeds are sown into wet soil. In soil prepared by the Tatura system, the percentage of aggregates < 0.5 mm diameter (as measured by dry-sieving) in the seed-bed was about half that found in commercially prepared seed-beds which were tilled up to 50 times when dry. With the Tatura system, the wetter the soil (up to 22% water content) when tilled, or the more passes (up to 4) of the implement at a water content of 22%, the less dust (< 0.5 mm diameter) and/or fewer clods (> 20 mm diameter) were formed. The macro-structure of the surface layer of soil tilled at different water contents by the Tatura system was also quantified statistically by the method of wax-impregnation. The macro-structures were compared at the 10 mm, 20 mm, 40 mm, 60 mm and 80 mm depths in beds of soil prepared for irrigated annual row-crops by a system which has been described previously. Within each treatment (21.7%; 19.0%; 11.6% water content at 0-100 mm depth at tillage), the linear porosity and mean pore-size each tended to decrease with depth to 40 mm, with no further change or slight decrease to 80 mm depth. In all treatments, the mean aggregate-size tended to increase with depth from 10 mm depth to 80 mm depth. The sizes of pores and aggregates varied across each bed and possibly depended on the position of tines within the bed at each pass at tillage. Water content at tillage led to small differences in structure of the beds of soil. Soil tilled at a water content slightly above the Casagrande Plastic Limit generally had slightly larger pores and aggregates than soil tilled at lower water contents.
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页码:561 / 576
页数:16
相关论文
共 18 条
[1]  
ADEM HH, 1982, AUSTR COUNTRY, V26, P62
[2]   PLOW-LAYER POROSITY AND SURFACE ROUGHNESS FROM TILLAGE AS AFFECTED BY INITIAL POROSITY AND SOIL MOISTURE AT TILLAGE TIME [J].
ALLMARAS, RR ;
BURWELL, RE ;
HOLT, RF .
SOIL SCIENCE SOCIETY OF AMERICA PROCEEDINGS, 1967, 31 (04) :550-&
[3]  
CHEPIL W. S., 1962, SOIL SCI SOC AMER PROC, V26, P4
[4]   BASIS FOR A PROCEDURE TO SPECIFY SOIL PHYSICAL-PROPERTIES OF A SEED BED FOR WHEAT [J].
COLLISGEORGE, N ;
LLOYD, JE .
AUSTRALIAN JOURNAL OF AGRICULTURAL RESEARCH, 1979, 30 (05) :831-846
[5]   INTERNAL STRUCTURE OF TILLED SOIL [J].
DEXTER, AR .
JOURNAL OF SOIL SCIENCE, 1976, 27 (03) :267-278
[6]   STRUCTURE OF A TILLED SOIL AS INFLUENCED BY TILLAGE, WHEAT CROPPING, AND RAINFALL [J].
DEXTER, AR ;
RADKE, JK ;
HEWITT, JS .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1983, 47 (03) :570-575
[7]   MACRO-STRUCTURE OF THE SURFACE-LAYER OF A SELF-MULCHING CLAY IN RELATION TO CEREAL STUBBLE MANAGEMENT [J].
DEXTER, AR ;
HEIN, D ;
HEWITT, JS .
SOIL & TILLAGE RESEARCH, 1982, 2 (03) :251-264
[8]   EFFECTS OF TILLAGE AND STUBBLE MANAGEMENT ON THE STRUCTURE OF A SWELLING SOIL [J].
HEWITT, JS ;
DEXTER, AR .
JOURNAL OF SOIL SCIENCE, 1980, 31 (02) :203-215
[9]  
HOYLE BJ, 1972, CALIF AGR, V26, P3
[10]  
LOVEDAY J, 1980, 1980 NAT SOILS C REV, P39