Clay spreading on water repellent sands in the south east of South Australia - promoting sustainable agriculture

被引:47
作者
Cann, MA [1 ]
机构
[1] Struan, Primary Ind & Resources, Naracoorte, SA 5271, Australia
关键词
water repellence; fine particle amendments; soil pH; moisture;
D O I
10.1016/S0022-1694(00)00205-5
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Water repellence is a serious land degradation issue and a constraint to productivity on approximately two million hectares across South Australia. Sandy soils that have poor coverage of pasture and crops lend themselves to the risk of wind erosion and loss of yields. A technique that has once seen highly unproductive pasture country now producing crops is 'clay spreading'. As with many discoveries, the ability of clay to counteract the effects of water repellent sand was unearthed by accident thirty years ago by Clem Obst, farmer at Mundulla, SE of South Australia. Today, approximately 37,000 ha of land in South Australia has been clay spread, of which 32,000 ha is in the SE of South Australia. The application of clay to water repellent sand increases the effectiveness of pre-emergent herbicides, amelioration of water repellency, improves the germination, establishment and yields of pasture plants and crops and nutrient and moisture retention in the topsoil. Water repellent sand pastures generally contain little, if any, legume content and produce as little as 400 kg/ha dry matter compared to clayed pastures (3250 kg/ha) which are sub-clover or lucerne based. Spreading clay has generally doubled cropping yields. The technique of clay spreading is continually being modified to enable landholders to attain maximum economic returns while ensuring the long-term sustainability of agriculture on water repellent sands. (C) 2000 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:333 / 341
页数:9
相关论文
共 13 条
[1]  
BOND R. D., 1964, AUSTRALIAN J SOIL RES, V2, P123, DOI 10.1071/SR9640123
[2]  
BOND RD, 1978, ADDITION CORES LOAM, P285
[3]  
Isbell R. F., 1996, The Australian soil classification.
[4]  
KEMPER WD, 1974, STRENGTH SOIL CRUSTS, V214, P31
[5]   COMPARISON OF METHODS FOR MEASURING SEVERITY OF WATER REPELLENCE OF SANDY SOILS AND ASSESSMENT OF SOME FACTORS THAT AFFECT ITS MEASUREMENT [J].
KING, PM .
AUSTRALIAN JOURNAL OF SOIL RESEARCH, 1981, 19 (04) :275-285
[6]  
KING PM, 1974, INTERNAL PUB S AUST, V26, P14
[7]   THE USE OF DISPERSIBLE CLAYS TO REDUCE WATER-REPELLENCY OF SANDY SOILS [J].
MASHUM, M ;
OADES, JM ;
TATE, ME .
AUSTRALIAN JOURNAL OF SOIL RESEARCH, 1989, 27 (04) :797-806
[8]  
MASHUM M, 1988, THESIS U ADELAIDE AU
[9]   EFFECTS OF SAND TYPE AND FINE PARTICLE AMENDMENTS ON EMERGENCE AND GROWTH OF SUBTERRANEAN CLOVER (TRIFOLIUM SUBTERRANEUM L) WITH PARTICULAR REFERENCE TO WATER RELATIONS [J].
ROBERTS, FJ .
AUSTRALIAN JOURNAL OF AGRICULTURAL RESEARCH, 1966, 17 (05) :657-+
[10]   WATER AND SOLUTE MOVEMENT IN A COARSE-TEXTURED WATER-REPELLENT FIELD SOIL [J].
VANDAM, JC ;
HENDRICKX, JMH ;
VANOMMEN, HC ;
BANNINK, MH ;
VANGENUCHTEN, MT ;
DEKKER, LW .
JOURNAL OF HYDROLOGY, 1990, 120 (1-4) :359-379