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当前位置: 首页 > 文章 > Soil physical quality as influenced by long-term fertilizer management under an intensive cropping system 国际农业与生物工程学报 2009,2 (1)
Position: Home > Articles > Soil physical quality as influenced by long-term fertilizer management under an intensive cropping system International Journal of Agricultural and Biological Engineering 2009,2 (1)

Soil physical quality as influenced by long-term fertilizer management under an intensive cropping system

作  者：
Zhangliu Du;Shufu Liu;Xiaoping Xiao;Guibiao Yang;Tao Re
单  位：
China Agricultural University;China Agricultural Universit;Soil and Fertilizer Institute of Hunan Province
关键词：
mineral fertilizer;manure;concentration;soc;rate;long-term fertilize
摘  要：
The influences of long-term fertilizer management on soil organic carbon (SOC) concentration and soil physical properties were investigated under an intensive rice production system in southern China. The experiment, initiated in 1986, has f ive treatments: unfertilized, mineral fertilizer alone, rice residues plus mineral fertilizer, low manure rate plus mineral fertilizer, and high manure rate plus mineral fertilizer. The cropping system consists of barley (Hordaum vulgare L.), early rice, and late rice ( Oryza sativa L. ), three crops in a year . In May 2006, after barley harvest, soil samples were collected from the 0-10 and 10-20 cm layers to determine SOC concentration , aggregate size distribution, bulk density ( r b ), saturated hydraulic conductivity ( K s ), and water characteristic curves (SWCC). The results indicated that manure significantly reduced r b , increased SOC concentration, soil aggregation, K s , transmission and storage porosity, as well as water retention capacity. Combined application of crop residue and mineral fertilizer also improved soil physical properties, but the improvement by mineral fertilizer alone was limited. Correlation analysis demonstrated that S, the slope of the SWCC at its inflection point , was closely associated with the selected physical parameters, suggesting S was an effective parameter for soil physical quality evaluation. Nevertheless, in applying the S - theory, a unified approach to define the residual water content should be considered.

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