CAJ | 학술논문

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 mS/cm下降到0.3 mS/cm以下；滴灌可使根区盐分下降至0.2 mS/cm，显著低于灌溉初始的盐分含量(P＜0.05)。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。
위료명학적관목숙토양수、염운이，세근분포급세근생물량동태，해문대목숙진행적관화만관시험，결과표명，만관수분집중재15 cm천층토양내차분포균균，함수솔재19.5%～20.5%지간。적관수분고치구집중재수평방향거적두15 cm，심도위40 cm적토층중，함수솔체도18.0%～20.0%。만관대0～25 cm심도토층염분림세작용명현，토수비1：5토양수제액적전도솔유관전적0.4～0.5 mS/cm하강도0.3 mS/cm이하；적관가사근구염분하강지0.2 mS/cm，현저저우관개초시적염분함량(P＜0.05)。여만관비교，적관목숙세근집중분포재수평방향거적두0～30 cm，수직심도0～50 cm범위내。생장계각시간절점적관세근총량고우만관，기평균치분별위211.6화198.3 g/m2。적관화만관각시간절점세근량표현출명현적파동，기범위분별재193.2～243.6화182.7～219.1 g/m2지간。재정개생장기내，적관활근량고우만관，차생장전기적관사근량변화교만관평은。활세근화사세근지간적주전사득량자정현출차소피창적상태，표명세근구유생장-조망-재생장적주기성。해연구가위적관기술재목숙재배상적응용제공삼고。
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 irrigation plots, soil moisture was concentrated in the upper 40 cm of the soil profile and within 30 cm on either side of the emitter of drip irrigation tapes, and the soil water content ranged between 18.0%and 20.0%. Flood irrigation leached salt to below the 30 cm depth. As a result, salinity in the 0-30 cm depth decreased from 0.4-0.5 mS/cm to 0.3 mS/cm or less. Drip irrigation significantly reduced the salinity to 0.2 mS/cm in the root zone. The narrower-deeper-type soil wetting pattern and desalted zone were formed in drip irrigation and alfalfa planted in this area has higher water content and lower salt content than flood irrigation, therefore drip irrigation provides excellent soil environment for alfalfa growth. While wider-shallower-type soil wetting pattern and desalted zone were formed in flood irrigation. Compared with the flood irrigation treatment, fine roots in the drip irrigation treatment were concentrated in the 0-50 cm depth and near to the emitter of drip irrigation tapes. Total fine roots biomass was greater in the drip irrigation treatment (212 g/m2) than that in the flood irrigation treatment (198 g/m2). Fine root biomass fluctuated during the growing season because of regrowth of alfalfa and harvest schedule. Fine root biomass ranged from 193 to 244 g/m2 in the drip irrigation treatment and from 183 g/m2 to 219 g/m2 in the flood irrigation treatment. During the entire growing period, live fine root biomass was greater in the drip irrigation treatment than that in the flood irrigation treatment. Live fine root biomass was fluctuated in flood and drip irrigation obviously, ranged from 73 to 139 g/m2 and 97 to 144 g/m2 respectively, During the early growth stages (from 2nd April to 18th July), the biomass of dead fine roots changed more smoothly in the drip irrigation treatment (ranged from 93 to 101 g/m2) than in the flood irrigation treatment(ranged from 96 to 125 g/m2), but the biomass of dead fine roots in drip irrigation was fluctuated from 72 to 102 g/m2 after 18th July. Biomasses of live and dead fine roots both changed continuously because of rapid turnover of fine roots, first increasing (growth), then decreasing (death and decomposition), and then increasing again (regrowth) . The results indicated that drip irrigation provide suitable soil condition for alfalfa growth by redistribution of soil water and salt, and the model of the wide-narrow row plantation with a distance of 15 cm+30 cm+15 cm between rows and drip irrigation is the optimal cultivation pattern of alfalfa.