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    不同密度和水分管理下毛白杨林分土壤水分特征

    Soil water characteristics of Populus tomentosa stands under different densities and water treatments

    • 摘要:
      目的 土壤水分是影响我国北方水分亏缺地区植被生长的重要因素,探究不同造林密度和水分管理下毛白杨林分的土壤水分状况,能为华北黄泛平原地区人工林土壤水分维持提供参考。
      方法 以不同造林密度(Ⅲ3 m × 3 m、Ⅱ3 m × 6 m、Ⅰ6 m × 6 m)和水分管理(滴灌FI、雨养NI)下的5种(FI、FI、NI、NI、NI)毛白杨林分为研究对象,在2021年生长季内(5、6、8和10月),采用烘干称重法测定各处理6 m剖面内的土壤含水量(SWC),研究不同处理土壤水分状况及土壤干层现象。
      结果 (1)各处理毛白杨林分浅土层(0 ~ 30 cm和30 ~ 100 cm)的SWC(5.62% ~ 15.53%)显著低于深土层(100 ~ 200 cm、200 ~ 400 cm和400 ~ 600 cm)(16.50% ~ 27.00%);林分SWC在0 ~ 240 cm垂直剖面内随深度增加而增加,并在240 ~ 260 cm(26.37% ~ 30.56%)和360 ~ 400 cm(22.79% ~ 33.00%)出现两个峰值,而400 ~ 600 cm变化平缓;(2)5种林分土壤均在10月最为湿润,平均SWC为20.16% ~ 23.16%;雨养条件下,不同密度毛白杨林分在6月最干燥,平均SWC为13.11% ~ 14.96%,滴灌减轻了30 cm以下土层SWC的季节变异程度;(3)不同水分管理下,高密度林分中深土层土壤水分状况最好(FI和NI深土层平均SWC分别为23.18%和21.13%),但雨季末(10月),NI土壤水分补偿量最高,达403.12 mm。在高密度和低密度林分中滴灌显著提高了林分0 ~ 30 cm土层的SWC,且增加了深土层土壤水分补偿量(FI较NI和FI较NI的储水量变化量分别提高了84.40%和173.99%),滴灌仅显著提高了高密度林分土壤储水量(P < 0.05);(4)滴灌和降雨均能缓解或消除不同密度林分在2 m深度内出现的可恢复性土壤干层现象。
      结论 根据本研究结果,建议在华北黄泛平原毛白杨大径材林培育过程中,以3 m × 3 m密度造林且于旱季(4—6月)辅以多频率滴灌充分灌溉,促进杨树人工林在快速生长期(2 ~ 4年)的林木生长并改善其深层土壤水分状况。待林分出现密度效应及深层土壤水消耗后,可通过间伐等措施在实现土壤水分维持的同时提高杨树人工林林地生产力。

       

      Abstract:
      Objective In water-deficit area of northern China, soil water content is a crucial factor affecting plant growth. Studying the soil water status of Populus tomentosa stands under different planting densities and water treatments can provide a reference basis for soil water maintenance of plantations in the North China Plain.
      Method Populus tomentosa plantations under five different planting densities (Ⅲ 3 m × 3 m, Ⅱ 3 m × 6 m and Ⅰ 6 m × 6 m) and water (drip irrigation, FI and rainfed, NI) treatments (FI, FI, NI, NI and NI) were selected in this study. During the growing season (May, June, August and October) in 2021, soil water content (SWC) within the 6 m-depth soil profile was measured using the drying-weighing method, soil water content conditions and the occurrence of dry soil layer (DSL) were investigated and compared among different treatments.
      Result (1) Shallow soil layers (0−30 cm and 30−100 cm, ranging from 5.62% to 15.53%) showed significantly lower SWC than the deep soil layers (100−200 cm, 200−400 cm, and 400−600 cm, ranging from 16.50% to 27.00%) in each treatment. The SWC in all stands increased with depth within the vertical profile of 0−240 cm, showing two peaks at 240−260 cm (26.37%−30.56%) and 360−400 cm (22.79%−33.00%), while the change of SWC at 400−600 cm was relatively gradual. (2) All five stands exhibited the highest soil water availability in October, with an average SWC from 20.16% to 23.16%. In rainfed treatment, soil was driest in June independent of planting density, the average SWC ranged from 13.11% to 14.96%. Drip irrigation treatment reduced the seasonal variation in SWC in the soil layer below 30 cm. (3) Under different water treatments, high density stands exhibited the highest soil water availabilities in the deep soil layers (average SWC of 23.18% for FI and 21.13% for NI). However, NI exhibited the highest soil water compensation at the end of the rainy season (October) of 403.12 mm. In both high and low density stands, SWC in the 0−30 cm soil layer was significantly increased by drip irrigation treatment, the compensation of soil water in the deep layers was also enhanced (the change in water storage was 84.40% in FI than in NI, and 173.99% higher in FI than in NI). Drip irrigation treatment only significantly improved soil water storage in high density stands (P < 0.05). (4) Both drip irrigation and precipitation effectively alleviated or eliminated the occurrence of recoverable DSL within 2 m-depth under different planting densities.
      Conclusion According to the results of this study, a 3 m × 3 m planting density with frequent full irrigation treatment during dry season (April to June) is recommended for the cultivation of large-diameter poplar plantation in the North China Yellow River Plain in order to achieve fast tree growth in the early growing stage (2−4 years) and improve water condition of the deep soil layers. After the occurrence of evident density effect and deep soil water content depletion, management practices like thinning can be implemented to maintain soil water production and enhance the productivity of poplar plantations.

       

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