人工草地建设是缓解内蒙古地区草地生存压力的必要途径,而水分短缺是该区人工草地建设中牧草生长的主要限制因素,适量的人工补水以实现牧草的高产节水是解决这一问题的关键。以当地主要牧草冰草和紫花苜蓿为研究对象,开展单播和混播条...人工草地建设是缓解内蒙古地区草地生存压力的必要途径,而水分短缺是该区人工草地建设中牧草生长的主要限制因素,适量的人工补水以实现牧草的高产节水是解决这一问题的关键。以当地主要牧草冰草和紫花苜蓿为研究对象,开展单播和混播条件下不同灌溉量对牧草产量、光合性能和水分利用效率影响的对比试验。研究结果表明:(1)豆禾混播有利于提高冰草和紫花苜蓿的产量;(2)8月初现蕾期是冰草和紫花苜蓿收割的最佳季节,此时牧草产量最高;(3)灌溉量达到田间持水量的45%(包含降雨量在内的单位面积灌溉量在7月初达到903.8 m3/hm2,在8月初达到1812.4 m3/hm2)是牧草高产节水的最佳补水选择;(4)6—8月水分胁迫更有利于提高牧草的长期水分利用效率(long-term water use efficiency,WUEL),开花期后补水对提高牧草WUEL的作用开始显著;(5)在牧草产量最高的8月初水分胁迫更有利于提高牧草的瞬时水分利用效率(instantaneous water use efficiency,WUEI),而在7月初光照强烈、水分蒸发量大时,较多地补水更有利于提高牧草的WUEI。展开更多
The woodland-steppe ecotone in the. southern Nei Mongol Plateau is located at the northern edge of the east Asian monsoon influences. A marked southeastern - northwestern (SE - NW) precipitation gradient exists in thi...The woodland-steppe ecotone in the. southern Nei Mongol Plateau is located at the northern edge of the east Asian monsoon influences. A marked southeastern - northwestern (SE - NW) precipitation gradient exists in this region. Quantitative reconstruction of palaeo-precipitation of this region is helpful to reveal the development of monsoon climate and to predict die future desertification. Based on modern vegetation and surface pollen studies, a pollen-precipitation transfer function in the study region was established. Pollen data from three sediment sequences within the ecotone were used to reconstruct palaeo-precipitation during the Holocene. The processes of precipitation changes in the three sequences were quite different. There was a tendency of precipitation declined from the onset of the Holocene to 1 100 a BP in Haoluku. But, in Liuzhouwan and Xiaoniuchang, both located south of Haoluku, the annual precipitation reached highest values during 7 800 - 6 200 a BP and 7 200 - 5 000 a BP, respectively. The influences of southwestern (SW) monsoon and the variances of topographical conditions have possibly caused these temporal-spatial variances.展开更多
文摘人工草地建设是缓解内蒙古地区草地生存压力的必要途径,而水分短缺是该区人工草地建设中牧草生长的主要限制因素,适量的人工补水以实现牧草的高产节水是解决这一问题的关键。以当地主要牧草冰草和紫花苜蓿为研究对象,开展单播和混播条件下不同灌溉量对牧草产量、光合性能和水分利用效率影响的对比试验。研究结果表明:(1)豆禾混播有利于提高冰草和紫花苜蓿的产量;(2)8月初现蕾期是冰草和紫花苜蓿收割的最佳季节,此时牧草产量最高;(3)灌溉量达到田间持水量的45%(包含降雨量在内的单位面积灌溉量在7月初达到903.8 m3/hm2,在8月初达到1812.4 m3/hm2)是牧草高产节水的最佳补水选择;(4)6—8月水分胁迫更有利于提高牧草的长期水分利用效率(long-term water use efficiency,WUEL),开花期后补水对提高牧草WUEL的作用开始显著;(5)在牧草产量最高的8月初水分胁迫更有利于提高牧草的瞬时水分利用效率(instantaneous water use efficiency,WUEI),而在7月初光照强烈、水分蒸发量大时,较多地补水更有利于提高牧草的WUEI。
文摘The woodland-steppe ecotone in the. southern Nei Mongol Plateau is located at the northern edge of the east Asian monsoon influences. A marked southeastern - northwestern (SE - NW) precipitation gradient exists in this region. Quantitative reconstruction of palaeo-precipitation of this region is helpful to reveal the development of monsoon climate and to predict die future desertification. Based on modern vegetation and surface pollen studies, a pollen-precipitation transfer function in the study region was established. Pollen data from three sediment sequences within the ecotone were used to reconstruct palaeo-precipitation during the Holocene. The processes of precipitation changes in the three sequences were quite different. There was a tendency of precipitation declined from the onset of the Holocene to 1 100 a BP in Haoluku. But, in Liuzhouwan and Xiaoniuchang, both located south of Haoluku, the annual precipitation reached highest values during 7 800 - 6 200 a BP and 7 200 - 5 000 a BP, respectively. The influences of southwestern (SW) monsoon and the variances of topographical conditions have possibly caused these temporal-spatial variances.
