CHANGES IN THE PHYSICAL-PROPERTIES OF A VERTISOL FOLLOWING AN IRRIGATION OF COTTON AS INFLUENCED BY THE PREVIOUS CROP

被引:23
作者
HULME, PJ
MCKENZIE, DC
ABBOTT, TS
MACLEOD, DA
机构
[1] UNIV NEW ENGLAND, DEPT AGRON & SOIL SCI, ARMIDALE, NSW 2351, AUSTRALIA
[2] NEW S WALES AGR & FISHERIES, HAYMARKET, NSW 2000, AUSTRALIA
[3] NEW S WALES AGR & FISHERIES BIOL & CHEM RES INST, RYDALMERE, NSW 2116, AUSTRALIA
来源
AUSTRALIAN JOURNAL OF SOIL RESEARCH | 1991年 / 29卷 / 03期
关键词
D O I
10.1071/SR9910425
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Structural degradation of Vertisols depresses cotton lint yield by extending the period of waterlogging following irrigation or heavy rainfall. Break crops such as wheat and safflower are often grown without irrigation to improve the macroporosity of degraded Vertisols, by encouraging deep cracking, after several years of cotton production. Investigations were made into the effects of cultivated fallow, wheat and safflower on soil structure, and the growth of a subsequent cotton crop. The tests reported in this paper, done over a 12-day period following irrigation, were: soil water content and potential, core and clod bulk density, air-filled porosity, an index of macropore continuity using Rhodamine dye, and penetration resistance. The results, when compared with established limits of aeration and penetration resistance to cotton root growth, indicate that soil physical conditions at 0.25 m should have impeded root growth regardless of water content. However, cotton roots continued to extract water in this hostile soil environment; this favourable performance was attributed to the better conditions for root growth in the interaggregate fissures than those within aggregates. Apart from water content, all indicators of soil structure were able to differentiate consistently between the three crop treatments to a depth of 0.25 m. Below 0.8 m, the cropped plots, particularly safflower, had lower water contents than the fallow plots.
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页码:425 / 442
页数:18
相关论文
共 47 条
[1]   FIELD EVIDENCE FOR A BI-POROUS SOIL-WATER REGIME IN CLAY SOILS [J].
ARMSTRONG, AC ;
ARROWSMITH, R .
AGRICULTURAL WATER MANAGEMENT, 1986, 11 (02) :117-125
[2]   COTTON ROOT-GROWTH AND SOIL-WATER EXTRACTION [J].
BLAND, WL ;
DUGAS, WA .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1989, 53 (06) :1850-1855
[3]  
Bruce R. R., 1986, Methods of soil analysis. Part 1. Physical and mineralogical methods, P663
[4]   SIMPLE METHOD FOR DETERMINING UNSATURATED CONDUCTIVITY FROM MOISTURE RETENTION DATA [J].
CAMPBELL, GS .
SOIL SCIENCE, 1974, 117 (06) :311-314
[5]   SHRINKAGE CHARACTERISTICS OF SOIL CLODS FROM A GREY CLAY UNDER INTENSIVE CULTIVATION [J].
CHAN, KY .
AUSTRALIAN JOURNAL OF SOIL RESEARCH, 1982, 20 (01) :65-68
[6]   MOISTURE REGIMES OF A CRACKING CLAY SOIL UNDER FURROW IRRIGATED COTTON [J].
CHAN, KY ;
HODGSON, AS .
AUSTRALIAN JOURNAL OF EXPERIMENTAL AGRICULTURE, 1981, 21 (112) :538-542
[7]  
CLAPP RB, 1978, WATER RESOUR RES, V14, P601, DOI 10.1029/WR014i004p00601
[8]   INFILTRATION AND STRUCTURAL CHANGES AS INFLUENCED BY INITIAL MOISTURE-CONTENT [J].
COLLISGEORGE, N ;
LAL, R .
AUSTRALIAN JOURNAL OF SOIL RESEARCH, 1971, 9 (02) :107-+
[9]   DEGRADATION AND RESTORATION OF SOIL STRUCTURE IN A CRACKING GREY CLAY USED FOR COTTON PRODUCTION [J].
DANIELLS, IG .
AUSTRALIAN JOURNAL OF SOIL RESEARCH, 1989, 27 (02) :455-469
[10]  
Danielson RE, 1967, IRRIGATION AGR LANDS