玉米品种对饱和土壤栽培和潮沼临时淹水的响应

Arlingga Ichwan Maulana, M. Ghulamahdi, I. Lubis
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引用次数: 4

摘要

玉米是世界上重要的粮食作物和饲料之一。农用地转为非农用地是玉米产量下降的主要原因之一。饱和土壤栽培(SSC)是一种连续灌溉,持续保持水深,使土层处于饱和状态的栽培技术。该技术可防止潮沼泽中黄铁矿氧化。本试验旨在研究饱和土壤栽培条件下临时淹水对玉米生长和产量的影响。该研究是在印度尼西亚占比省Tanjung Jabung Timur的Rantau Rasau的Karya Bhakti村进行的。试验采用3个重复的分割图设计。主要地块为淹水条件,包括:1)从种植至收获时段连续饱和土壤条件(对照);2)0 ~ 10 DAP(种植后d)饱和土壤条件+ 11 ~ 13 DAP淹水+ 14 ~ 28 DAP饱和土壤条件+ 29 ~ 31 DAP淹水+ 32 DAP饱和土壤条件至收获时段。副标题是玉米品种,“Sukmaraga”、“Bisma”、“Pioneer 27”和“Bima 20”。“先锋27号”的生产率最高,为9.33 t.ha-1。耐暂涝性中等的玉米品种是“苏马拉加”和“比斯玛”,而“先锋27号”和“比马20号”对暂涝敏感。
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Response of Corn Varieties under Saturated Soil Culture and Temporary Flooding in Tidal Swamp
Corn is one of the important food crops and feeds in the world. Conversion of agricultural land into non-agricultural land is one of the major causes of the decline in corn production. Saturated soil culture (SSC) is a cultivation technology that gives continuous irrigation and maintains water depth constantly and makes soil layer in saturated condition. This technology can prevent pyrite oxidation in the tidal swamp. This research aimed to study the effect of temporary fl ooding under saturated soil culture on the growth and productivity of corn. The research was conducted at Karya Bhakti village, Rantau Rasau, Tanjung Jabung Timur, Jambi Province, Indonesia. The experiment used a split plot design with three replications. The main plot is fl ooding condition, consisted of 1) saturated soil condition continuously, from planting until harvesting time (as control), and 2) saturated soil condition from 0 to 10 DAP (Days after Planting) + fl ooding from 11 to 13 DAP + saturated soil condition from 14 to 28 DAP + fl ooding from 29-31 DAP + saturated soil condition from 32 DAP until harvesting time. The subplot is corn variety, “Sukmaraga”, “Bisma”, “Pioneer 27”, and “Bima 20”. “Pioneer 27” had the highest productivity of 9.33 t.ha-1. Corn varieties with moderate tolerance to temporary fl ooding were “Sukmaraga” and “Bisma”, whereas “Pioneer 27” and “Bima 20” are sensitive to fl ooding.
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