1. 西南大学资源环境学院,重庆,400716
2. ,兰州
3. 农业部耕地保育重点实验室 国家紫色土肥力与肥料效益监测站,重庆,400716
纸质出版:2017
移动端阅览
柴冠群, 赵亚南, 黄兴成, 等. 不同炭基改良剂提升紫色土蓄水保熵能力[J]. 水土保持学报, 2017,(1):296-302.
Effects of Different Carbonaceous Conditioners on Water Retention Capacity of Purple Soil[J]. 2017, (1): 296-302.
柴冠群, 赵亚南, 黄兴成, 等. 不同炭基改良剂提升紫色土蓄水保熵能力[J]. 水土保持学报, 2017,(1):296-302. DOI: 10.13870/j.cnki.stbcxb.2017.01.049.
Effects of Different Carbonaceous Conditioners on Water Retention Capacity of Purple Soil[J]. 2017, (1): 296-302. DOI: 10.13870/j.cnki.stbcxb.2017.01.049.
通过连续2年田间试验,研究了5种改良剂:秸秆、有机肥、生物炭、炭基改良剂I和炭基改良剂Ⅱ对紫色丘陵区坡耕地土壤水分库容、孔隙度和团聚体组成及稳定性的影响,分析了土壤水分特征参数与孔隙度和团聚体组成的关系,以期为紫色土区水土保持和土壤改良提供科学依据。与不施改良剂(对照)相比,5种炭基改良剂都能提高土壤对降水的截存和保贮能力,显著提高了土壤饱和含水量、田间持水量、水分总库容、有效水库容及重力水库容,降低了土壤凋萎点含水量和无效水库容;不同改良剂提升作用大小为改良剂Ⅱ>改良剂I>生物炭>有机肥>秸秆>对照。施用改良剂I、改良剂Ⅱ、生物炭和有机肥显著提高了土壤孔隙度,降低了土壤容重,秸秆的效果不显著。施用炭基改良剂降低了<0.25 mm的微团聚体含量,促进了小团聚体向大团聚体的转化,其中对粒径>5 mm的机械稳定性大团聚体提升幅度最大,比对照提高14.5%~60.7%;5种炭基改良剂都显著提高了团聚体的平均重量直径及稳定性指数,以炭基改良剂I、Ⅱ和生物炭的作用效果最大。土壤总库容、重力水库容和有效水库容与总孔隙度和毛管孔隙度以及土壤大团聚体含量呈正相关,而与土壤非毛管孔隙度和小团聚体呈负相关,土壤蓄水保水能力与土壤团聚体组成和孔隙度密切相关。因此,施用炭基改良剂通过促进土壤团聚作用,提高大团聚体含量和土壤孔隙度,进而增大土壤持水量和土壤有效水库容,是改善紫色土结构和提高紫色土坡耕地保水蓄水能力的有效措施。
Slope cropland of purple soil was the main part of agricultural production in the hilly region of Sichuan basin
where there are large precipitation and concentration in summer and autumn. When the rainstorm occurred
the water and soil loses easily
which led to shallowing soil layer
decreasing the soil moisture and seasonal drought occurrence. Some researchers found that the straw
the biochar and the organic fertilizer were able to increase the soil porosity and enlarge the soil moisture
but there was rare in the slope cropland of purple soil. Thus
to investigate the effect of soil ameliorants on the composition and stability of soil aggregate and moisture storage capacity of slope cropland in purple hilly area
two-year filed experiment was conducted by employing five kinds of soil ameliorants including straw
organic fertilizer
biochar
carbonaceous ameliorant I and Ⅱ. The results showed that all these five carbonaceous ameliorants were also observed to have the ability on enhancing the sequestration and storage of soil for precipitation
which could further markedly increase the saturated soil moisture content and maximum effective water and flood detention storage and decrease the water content of wilting point. The effect of these five soil ameliorants on the maximum effective capacity followed the trend: Carbonaceous ameliorant Ⅱ>carbonaceous ameliorant I>biochar>manure>straw>CK. The soil bulk density and soil porosity also received valid improvement after applying these ameliorants (besides straw)
which significantly decreased and increased
respectively. In addition
the mechanical stability and the water stable aggregate content of soil with particle size >0.25mm significantly increased after soil ameliorants applied
while the micro-aggregate (<0.25mm) content decreased
suggested that the soil ameliorant could promote the conversion of small aggregate to large aggregate with the best promotion observed for >5mm particle (increased 14.5 to 60.7% compared with the contrast). Employing these soil ameliorants had obvious effect (followed the trend: carbonaceous ameliorant I≈carbonaceous ameliorant Ⅱ>biochar>organic fertilizer>straw>control) on increasing the average weight diameter and stability index of aggregate. Correlative analysis showed that there was a positive correlation between total storage capacity
active storage capacity
flood detention storage capacity and total soil porosity
capillary porosity
content of large aggregate
and there was negative correlation with non-capillary porosity and content of small aggregate. Therefore
there was close relation between soil moisture preservation and soil porosity. Applying soil carbonaceous ameliorant was an important measure to improve the structure of purple soil and increase the ability of moisture holding and anti-erosion of purple sloping cropland by promoting the conversion of small aggregate to large one
decreasing the soil bulk density
increasing the soil porosity and enlarging the soil moisture holding and the soil effective water storage
which prevented sloping land from the damage of local seasonal drought. Moreover
the limiting factor of low soil moisture preservation in slope cropland of purple hilly area might be low organic matter content.
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