Managed Aquifer Recharge of Monsoon Runoff Using Village Ponds: Performance Assessment of a Pilot Trial in the Ramganga Basin, India

The managed aquifer recharge (MAR) of excess monsoonal runoff to mitigate downstream flooding and enhance groundwater storage has received limited attention across the Indo-Gangetic Plain of the Indian subcontinent. Here, we assess the performance of a pilot MAR trial carried out in the Ramganga bas...

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Main Authors: Mohammad Faiz Alam, Paul Pavelic, Navneet Sharma, Alok Sikka
Format: Article
Language:English
Published: MDPI AG 2020-04-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/12/4/1028
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spelling doaj-f76f4a3b97e7410daedcdbb1b322a8ed2020-11-25T02:21:57ZengMDPI AGWater2073-44412020-04-01121028102810.3390/w12041028Managed Aquifer Recharge of Monsoon Runoff Using Village Ponds: Performance Assessment of a Pilot Trial in the Ramganga Basin, IndiaMohammad Faiz Alam0Paul Pavelic1Navneet Sharma2Alok Sikka3International Water Management Institute, New Delhi 110012, IndiaInternational Water Management Institute, Vientiane 4199, LaosInternational Water Management Institute, New Delhi 110012, IndiaInternational Water Management Institute, New Delhi 110012, IndiaThe managed aquifer recharge (MAR) of excess monsoonal runoff to mitigate downstream flooding and enhance groundwater storage has received limited attention across the Indo-Gangetic Plain of the Indian subcontinent. Here, we assess the performance of a pilot MAR trial carried out in the Ramganga basin in India. The pilot consisted of a battery of 10 recharge wells, each 24 to 30 m deep, installed in a formerly unused village pond situated adjacent to an irrigation canal that provided river water during the monsoon season. Over three years of pilot testing, volumes ranging from 26,000 to 62,000 m<sup>3</sup> were recharged each year over durations ranging from 62 to 85 days. These volumes are equivalent to 1.3–3.6% of the total recharge in the village, and would be sufficient to irrigate 8 to 18 hectares of rabi season crop. High inter-year variation in performance was observed, with yearly average recharge rates ranging from 430 to 775 m<sup>3</sup> day<sup>−1</sup> (164–295 mm day<sup>−1</sup>) and overall average recharge rates of 580 m<sup>3</sup> day<sup>−1</sup> (221 mm day<sup>−1</sup>). High intra-year variation was also observed, with recharge rates at the end of recharge period reducing by 72%, 88% and 96% in 2016, 2017 and 2018 respectively, relative to the initial recharge rates. The observed inter- and intra-year variability is due to the groundwater levels that strongly influence gravity recharge heads and lateral groundwater flows, as well as the source water quality, which leads to clogging. The increase in groundwater levels in response to MAR was found to be limited due to the high specific yield and transmissivity of the alluvial aquifer, and, in all but one year, was difficult to distinguish from the overall groundwater level rise due to a range of confounding factors. The results from this study provide the first systematic, multi-year assessment of the performance of pilot-scale MAR harnessing village ponds in the intensively groundwater irrigated, flood prone, alluvial aquifers of the Indo-Gangetic Plain.https://www.mdpi.com/2073-4441/12/4/1028managed aquifer rechargeUnderground Transfer of Floods for Irrigationdroughtsfloodsgroundwater depletion
collection DOAJ
language English
format Article
sources DOAJ
author Mohammad Faiz Alam
Paul Pavelic
Navneet Sharma
Alok Sikka
spellingShingle Mohammad Faiz Alam
Paul Pavelic
Navneet Sharma
Alok Sikka
Managed Aquifer Recharge of Monsoon Runoff Using Village Ponds: Performance Assessment of a Pilot Trial in the Ramganga Basin, India
Water
managed aquifer recharge
Underground Transfer of Floods for Irrigation
droughts
floods
groundwater depletion
author_facet Mohammad Faiz Alam
Paul Pavelic
Navneet Sharma
Alok Sikka
author_sort Mohammad Faiz Alam
title Managed Aquifer Recharge of Monsoon Runoff Using Village Ponds: Performance Assessment of a Pilot Trial in the Ramganga Basin, India
title_short Managed Aquifer Recharge of Monsoon Runoff Using Village Ponds: Performance Assessment of a Pilot Trial in the Ramganga Basin, India
title_full Managed Aquifer Recharge of Monsoon Runoff Using Village Ponds: Performance Assessment of a Pilot Trial in the Ramganga Basin, India
title_fullStr Managed Aquifer Recharge of Monsoon Runoff Using Village Ponds: Performance Assessment of a Pilot Trial in the Ramganga Basin, India
title_full_unstemmed Managed Aquifer Recharge of Monsoon Runoff Using Village Ponds: Performance Assessment of a Pilot Trial in the Ramganga Basin, India
title_sort managed aquifer recharge of monsoon runoff using village ponds: performance assessment of a pilot trial in the ramganga basin, india
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2020-04-01
description The managed aquifer recharge (MAR) of excess monsoonal runoff to mitigate downstream flooding and enhance groundwater storage has received limited attention across the Indo-Gangetic Plain of the Indian subcontinent. Here, we assess the performance of a pilot MAR trial carried out in the Ramganga basin in India. The pilot consisted of a battery of 10 recharge wells, each 24 to 30 m deep, installed in a formerly unused village pond situated adjacent to an irrigation canal that provided river water during the monsoon season. Over three years of pilot testing, volumes ranging from 26,000 to 62,000 m<sup>3</sup> were recharged each year over durations ranging from 62 to 85 days. These volumes are equivalent to 1.3–3.6% of the total recharge in the village, and would be sufficient to irrigate 8 to 18 hectares of rabi season crop. High inter-year variation in performance was observed, with yearly average recharge rates ranging from 430 to 775 m<sup>3</sup> day<sup>−1</sup> (164–295 mm day<sup>−1</sup>) and overall average recharge rates of 580 m<sup>3</sup> day<sup>−1</sup> (221 mm day<sup>−1</sup>). High intra-year variation was also observed, with recharge rates at the end of recharge period reducing by 72%, 88% and 96% in 2016, 2017 and 2018 respectively, relative to the initial recharge rates. The observed inter- and intra-year variability is due to the groundwater levels that strongly influence gravity recharge heads and lateral groundwater flows, as well as the source water quality, which leads to clogging. The increase in groundwater levels in response to MAR was found to be limited due to the high specific yield and transmissivity of the alluvial aquifer, and, in all but one year, was difficult to distinguish from the overall groundwater level rise due to a range of confounding factors. The results from this study provide the first systematic, multi-year assessment of the performance of pilot-scale MAR harnessing village ponds in the intensively groundwater irrigated, flood prone, alluvial aquifers of the Indo-Gangetic Plain.
topic managed aquifer recharge
Underground Transfer of Floods for Irrigation
droughts
floods
groundwater depletion
url https://www.mdpi.com/2073-4441/12/4/1028
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