为了明确滴灌苜蓿土壤水、盐运移,细根分布及细根生物量动态,该文对苜蓿进行滴灌和漫灌试验,结果表明,漫灌水分集中在15 cm浅层土壤内且分布均匀,含水率在19.5%~20.5%之间。滴灌水分高值区集中在水平方向距滴头15 cm,深度为40 cm的土层中,含水率达到18.0%~20.0%。漫灌对0~25 cm深度土层盐分淋洗作用明显,土水比1:5土壤水提液的电导率由灌前的0.4~0.5 m S/cm下降到0.3 m S/cm以下;滴灌可使根区盐分下降至0.2 m S/cm,显著低于灌溉初始的盐分含量(P0.05)。与漫灌比较,滴灌苜蓿细根集中分布在水平方向距滴头0~30 cm,垂直深度0~50 cm范围内。生长季各时间节点滴灌细根总量高于漫灌,其平均值分别为211.6和198.3 g/m2。滴灌和漫灌各时间节点细根量表现出明显的波动,其范围分别在193.2~243.6和182.7~219.1 g/m2之间。在整个生长期内,滴灌活根量高于漫灌,且生长前期滴灌死根量变化较漫灌平稳。活细根和死细根之间的周转使得两者呈现出此消彼涨的状态,表明细根具有生长-凋亡-再生长的周期性。该研究可为滴灌技术在苜蓿栽培上的应用提供参考。
Drip irrigation is being effectively used for alfalfa production in arid northwest China. The objectives of this paper were:i) to compare the effects of flood and drip irrigation on the spatial distribution of water and salt;ii) to compare effects of biomass, spatial distribution and dynamics of fine roots of alfalfa on the movement of water and salt in the soil profile under flood and drip irrigation. From May to October 2012, the plot experiments were carried out in Xinjiang Province. Flood irrigation (irrigation quantity is 4 600 m3/hm2) and drip irrigation treatments were set up (irrigation quantity is 4 200 m3/hm2), alfalfa planted in wide-narrow row plantation with a distance of 15 cm + 30 cm + 15 cm between rows. The results showed that soil water in the flood irrigation treatment was concentrated in the upper 15 cm of the soil profile. Furthermore, the soil water content was uniformly distributed across the plots, ranging between 19.5% and 20.5%. In the drip irrigatio