灌溉盐化环境下小麦根区盐分动态与收支

Parmanand Kumar, A. Sarangi, D. Singh
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摘要

植物生长受到根区盐沉积的不利影响,需要明智的灌溉水管理来提高灌溉盐碱化环境下的生产力。为研究小麦根区盐沉积及其后续淋溶,以4个小麦品种(3个耐盐品种KRL-210 (V)、KRL-1-4 (V)和1个不耐盐品种HD- 2894 (V)为材料,在4 dS m(S)的人工配制4-1-1-1灌溉水条件下进行了试验。印度农业研究所(IARI)研究农场2009-10年和2010-11年旱季地下水盐度在1.45 ~ 1.7 dS m(S)之间变化的8 dS m(S)和12 dS m(S)。-1试验前土壤盐度(EC)在rabi2009 -1:2-1 - 10期间为0.2 dS / m,在rabi2010-11期间为0.26 ~ 0.95 dS / m。2009-10年和2010-11年盐碱水对土壤的总盐诱导量分别为70.15 -1-1吨和55.6吨。处理小区根区盐-1沉积量最大(2009-10和2010-11年分别为17.04和22.97 t ha),处理水平最小。41建立了小麦品种的生产函数,耐盐品种和不耐盐品种的2决定系数(R)分别为0.98 ~ 0.99和0.94。此外,还估计最大的盐沉积在土壤表层(15cm), S, S,砂处理水平的盐浸出分别为65%,63%,123,452%和48%,分别来自根区。然而,这项研究将有助于计算在灌溉盐碱化环境中提高生产力的浸出需求。
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Salt Dynamics and Budgeting in the Root Zone of Wheat under Irrigated Saline Environment
Plant growth is adversely affected by salt deposition in the root zone and requires judicious irrigation water management for enhancing productivity in an irrigated saline environment. To study the salt deposition and subsequent leaching of salts below the root zone of wheat, an experiment with four wheat cultivars (viz. three salt-tolerant KRL-210 (V), KRL-1-4 (V), and 12one salt non-tolerant HD- 2894 (V) were taken for the experiment under artificially prepared 4-1-1-1irrigation water with salinity levels of 4 dS m(S), 8 dS m(S) and 12 dS m(S) besides the 234-1varying salinity of the groundwater from 1.45 to 1.7 dS m(S) during rabiseasons of 2009-10 and 12010-11 at the research farm of Indian Agricultural Research Institute (IARI), New Delhi, India. -1 The soil salinity (EC) was 0.2 dS mbefore the conduction of the experiment during rabi 2009-1:2-1 10 and varied from 0.26 to 0.95 dS mduring rabi2010-11. The total salt-induced in soil was 70.15 -1-1 t haand 55.6 t hafor rabi2009-10 and 2010-11 respectively by saline irrigation water. The salt -1deposition in the crop root zone was observed at maximum (i.e., 17.04 and 22.97 t ha during rabi2009-10 and 2010-11, respectively) for Streated plots and minimum in Streatment levels. 41The production functions for wheat varieties were developed and the coefficient of 2determination (R) was 0.98 to 0.99 and 0.94 for salt-tolerant and salt non-tolerant varieties, respectively. Moreover, it was also estimated that the maximum salt was deposited on the top soil layer (15cm) and the leaching of salts from S, S, Sand Streatments levels was 65%, 63%, 123,452%, and 48% salts, respectively from the root zone. However, this study would assist in the computation of leaching requirements for enhancing productivity in irrigated saline environments.
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