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Effects of straw mulch and buried straw on soil moisture and salinity in relation to sunflower growth and yield.

机译:秸秆覆盖和秸秆掩埋对土壤水分和盐分的影响与向日葵的生长和产量有关。

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Salt accumulation in the root zone can be controlled by reducing the upward movement of salts and evaporation in arid areas of China. This paper aimed to examine the effects of the combined application of straw mulch and buried straw layer on soil moisture, soil salinity and growth of sunflower (Helianthus annuus L.) plants. A three-year field experiment was conducted in the Hetao Irrigation District, Inner Mongolia, China. Three field management practices were studied: deep tillage with no mulch (CK), deep tillage with straw mulch (SM) and combined application of straw mulch and burying of a maize straw layer (12 t ha-1) at a depth of 40 cm (SM+SL). Except in the second half of the first growing season, soil moisture at the 0-40 cm depth was higher with SM+SL and SM than CK. Also the topsoil (0-20 cm) moisture during the early growth period under SM+SL was higher than that under SM by 1.6-9.9% in 2011 and 1.6-3.4% in 2013, but the value for SM+SL was 2.1-10.4% higher than that for SM during the whole growth period of 2012. Compared with SM, the topsoil salinity under SM+SL decreased by 5.4-23.0% in 2011, 0.7-19.8% in 2012 and 4.5-31.6% in 2013 but these two mulch treatments moderately increased the soil salinity in the subsoil (20-40 cm) layer compared with CK. Furthermore, SM+SL promoted sunflower growth, as indicated by taller plants and greater leaf area index. The highest sunflower shoot biomass was always obtained from the SM+SL treatment. Averaged across the three years, SM+SL increased the shoot biomass by 4.8% compared to SM and 20.8% compared to CK. The SM+SL may be an effective saline soil management practice in the Hetao Irrigation District and other similar ecological areas.
机译:可以通过减少中国干旱地区盐分的向上运动和蒸发来控制根区的盐分积累。本文旨在研究秸秆覆盖与秸秆掩埋层联合施用对向日葵植物土壤水分,盐分和生长的影响。在中国内蒙古河套灌区进行了为期三年的野外试验。研究了三种田间管理措施:无覆盖深耕(CK),秸秆覆盖深耕(SM)以及秸秆覆盖与玉米秸秆层掩埋相结合的应用(12 t ha -1 ),深度为40厘米(SM + SL)。除了在第一个生长季的后半段,SM + SL和SM的0-40 cm深度的土壤湿度高于CK。同样,SM + SL生育初期的表层土壤(0-20厘米)含水量比SM较高,2011年为1.6-9.9%,2013年为1.6-3.4%,但SM + SL的值为2.1-在2012年的整个生育期内,比SM高10.4%。与SM相比,SM + SL下的表层土壤盐度在2011年下降了5.4-23.0%,在2012年下降了0.7-19.8%,在2013年下降了4.5-31.6%,但是这些与CK相比,两次覆盖处理均适度增加了下层土壤(20-40 cm)的土壤盐分。此外,如更高的植物和更大的叶面积指数所示,SM + SL促进了向日葵的生长。始终从SM + SL处理中获得最高的向日葵芽生物量。三年平均来看,SM + SL与SM相比增加了4.8%,与CK相比增加了20.8%。在河套灌区和其他类似的生态地区,SM + SL可能是一种有效的盐渍土壤管理实践。

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