He Pingru, Li Jingang, Yu Shuang'en, Ma Tao, Ding Jihui, Zhang Fucang, Chen Kaiwen, Guo Shuaishuai, Peng Suhan
College of Agricultural Science and Engineering, Hohai University, Nanjing 210098, China.
Key Laboratory of Agricultural Soil and Water Engineering in Arid and Semiarid Areas of Ministry of Education, Northwest A&F University, Yangling 712100, China.
Plants (Basel). 2023 Feb 9;12(4):791. doi: 10.3390/plants12040791.
Water deficiency, together with soil salinization, has been seriously restricting sustainable agriculture around the globe for a long time. Optimal soil moisture regulation contributes to the amelioration of soil water and salinity for crops, which is favorable for plant production. A field experiment with five soil water lower limit levels (T1: 85% FC, T2: 75% FC, T3: 65% FC, T4: 55% FC, and T5: 45% FC, where FC is the field capacity) was conducted in southern Xinjiang in 2018 to investigate the responses of soil water-salt dynamics and cotton performance to soil moisture regulation strategies. The results indicated that in the horizontal direction, the farther away the drip irrigation belt, the lower the soil moisture content and the greater the soil salinity. In the vertical direction, the soil moisture and soil salinity increased first and then decreased with an increase in soil depth after irrigation, and the distribution was similar to an ellipse. Moreover, the humid perimeter of soil water and the leaching range of soil salt increased with a decrease in the soil moisture lower limit. Though more soil salt was leached out for the T5 treatment at the flowering stage due to the higher single irrigation amount, soil salinity increased again at the boll setting stage owing to the long irrigation interval. After the cotton was harvested, soil salt accumulated in the 0-100 cm layer and the accumulation amount followed T3 > T5 > T1 > T2 > T4. Moreover, with a decline of soil moisture lower limit, both plant height and nitrogen uptake decreased significantly while the shoot-root ratio increased. Compared with the yield (7233.2 kg·hm) and water use efficiency (WUE, 1.27 kg·m) of the T1 treatment, the yield for the T2 treatment only decreased by 1.21%, while the WUE increased by 10.24%. Synthetically, considering the cotton yield, water-nitrogen use efficiency, and soil salt accumulation, the soil moisture lower limit of 75% FC is recommended for cotton cultivation in southern Xinjiang, China.
长期以来,缺水以及土壤盐碱化一直严重制约着全球可持续农业的发展。优化土壤水分调控有助于改善作物生长的土壤水分和盐分状况,有利于作物生产。2018年在新疆南部进行了一项田间试验,设置了五个土壤水分下限水平(T1:85% 田间持水量,T2:75% 田间持水量,T3:65% 田间持水量,T4:55% 田间持水量,T5:45% 田间持水量,其中田间持水量用FC表示),以研究土壤水盐动态和棉花生长性能对土壤水分调控策略的响应。结果表明,在水平方向上,距滴灌带越远,土壤含水量越低,土壤盐分越高。在垂直方向上,灌溉后土壤水分和土壤盐分随土壤深度增加先升高后降低,其分布类似于椭圆形。此外,土壤水分湿润周长和土壤盐分淋洗范围随土壤水分下限的降低而增大。虽然T5处理在开花期因单次灌水量较大而淋洗出较多土壤盐分,但在结铃期由于灌溉间隔时间长,土壤盐分又有所增加。棉花收获后,0-100 cm土层土壤盐分积累,积累量顺序为T3>T5>T1>T2>T4。此外,随着土壤水分下限的降低,株高和氮素吸收量显著降低,而茎叶根比增加。与T1处理的产量(7233.2 kg·hm)和水分利用效率(WUE,1.27 kg·m)相比,T2处理的产量仅降低了1.21%,而WUE提高了10.24%。综合考虑棉花产量、水氮利用效率和土壤盐分积累情况,建议中国新疆南部棉花种植的土壤水分下限为75% 田间持水量。