Статті в журналах з теми "Gangetic Plains"

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1

NAVEEN P. SINGH, SURENDRA SINGH, BHAWNA ANAND, and P.C. Ranjith. "Assessing the impact of climate change on crop yields in Gangetic Plains Region, India." Journal of Agrometeorology 21, no. 4 (November 10, 2021): 452–61. http://dx.doi.org/10.54386/jam.v21i4.280.

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Against the increasing vulnerability of agriculture and farm livelihoods to climate change, the study attempted to analyse the trend in climate variables and their impact on major crop yields during the period from 1966-2011, across 4 agro-climatic zones forming Gangetic Plains Region. A rising trend was observed in annual and seasonal (kharif and rabi) mean maximum and minimum temperature across the zones. Rainfall on the other hand, showed a declining trend. Overall, climate change adversely impacted crop yield, but the magnitudes of such effects vary spatially. The results reveal that rice and wheat yield will decline in the entire Gangetic region. By 2050s, maize yield will be higher by 6 percent in Lower Gangetic Plains; pearl millet will increase by 15 percent and rapeseed & mustard by 3.8 percent in Trans-Gangetic Plains. Amongst the crops, sugarcane yield was the most impacted to climate change and is expected to reduce by 21 percent in Middle Gangetic Plains towards end of the century. Hence, there is a need to formulate sustainable adaptation measures and practices suitable to location-specific needs for enhancing climate resiliency and capacity of agricultural system to withstand climatic shocks.
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2

KASHYAPI, A., A. L. KOPPAR, and A. P. HAGE. "Crop specific requirement of growing degree days and agrometeorological indices in rice growing zones." MAUSAM 61, no. 4 (November 27, 2021): 569–76. http://dx.doi.org/10.54302/mausam.v61i4.915.

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The spatial and temporal distributions of heat unit and various agrometeorological indices for the rice crop, are studied in this paper. Eight ET – stations were selected from six rice growing zones, viz., Canning (in lower Gangetic plains), Bikramganj and Varanasi (in middle Gangetic plains), Ludhiana (in trans Gangetic plains), Ranchi, Shymakhunta (in eastern plateau and hills), Annamalai Nagar (in east coast plains and hill region) and Pattambi (in western plains and ghat region). Eleven crop growth stages were identified for this study, viz., germination, nursery seedling, transplanting, tillering, active tillering, lag phase, panicle initiation, flowering, grain formation, grain maturity and harvesting, the duration of each of the growth stages varied widely, station wise. Daily data were collected growth stagewise for latest available five years and the mean values were computed for the derived parameters, viz., the crop requirements of heat unit, agroclimatic rainfall index (ARI), yield moisture index (YMI), aridity index (AI). The study revealed that for rice crop the total degree days requirement varied from 1706 degree – days (at Ranchi) to 2815 degree – days (at Shymakhunta). It showed primary peak (with 16.7 % of total requirement) at active tillering stage. The ARI values were mostly higher than 100 per cent. The mean YMI values varied widely from 477 mm (at Bikramganj) to 1523 mm (at Pattambi). The values showed main peak at active tillering stage. The AI values showed moderate aridity at early growth stages, which increased at advanced crop growth stages.
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3

Rawat, Krishna Kumar, Afroz Alam, and Praveen Kumar Verma. "Checklist of mosses (Bryophyta) of Gangetic Plains, India." Bangladesh Journal of Plant Taxonomy 23, no. 2 (December 28, 2016): 97–106. http://dx.doi.org/10.3329/bjpt.v23i2.30818.

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An updated account of 79 taxa of mosses of Gangetic plains, representing 40 genera and 19 families, is provided. The family Pottiaceae with 17 taxa belonging to 9 genera appears most dominant and diversified family in the area while at generic level, the genus Fissidens (Fissidentaceae) with 19 species shows maximum diversity, followed by Hyophila and Physcomitrium each with five species.Bangladesh J. Plant Taxon. 23(2): 97-106, 2016 (December)
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4

TOMAR, K. P. "Chemistry of pedogenesis in Indo-Gangetic alluvial plains." Journal of Soil Science 38, no. 3 (September 1987): 405–14. http://dx.doi.org/10.1111/j.1365-2389.1987.tb02275.x.

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5

White, J. W., and A. Rodriguez-Aguilar. "An Agroclimatological Characterization of the Indo-Gangetic Plains." Journal of Crop Production 3, no. 2 (January 2001): 53–65. http://dx.doi.org/10.1300/j144v03n02_03.

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6

Nayak, Gourav, Ashwini Kumar, Srinivas Bikkina, Shani Tiwari, Suhas S. Sheteye, and A. K. Sudheer. "Carbonaceous aerosols and their light absorption properties over the Bay of Bengal during continental outflow." Environmental Science: Processes & Impacts 24, no. 1 (2022): 72–88. http://dx.doi.org/10.1039/d1em00347j.

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7

Sharma, Prashant, Manoj Singh, Kamlesh Verma, and Saroj Kumar Prasad. "Soil weed seedbank under different cropping systems of middle Indo-Gangetic Plains." Plant, Soil and Environment 68, No. 11 (November 28, 2022): 542–51. http://dx.doi.org/10.17221/162/2022-pse.

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Trees on agricultural fields can have a positive or negative impact on weed seedbank (WSB) due to diverse environmental and soil characteristics. Therefore, soil samples were drawn in six cropping systems [two agroforest systems (AFS): guava, mango; three horticulture systems (HCS): guava, mango, Indian gooseberry; and annual crop system (ACS)] at two landscape positions (lowland and upland) and two soil depths (0–15 cm and 15–30 cm) using factorial randomised block design each replicated three times. Results showed that guava-AFS had the highest WSB of different categories in general and individual weed species in particular, except for Eragrostis pilosa and Dactyloctenium aegyptium. Simultaneously, guava-AFS also showed the maximum Shannon-Weaver, species richness and Simpson index and was low in Whittaker statistics (βW). The species evenness varied non-significantly with the cropping systems. Similarly, the landscape position had no discernible effect on any weed diversity indices; however lowland landscape position was dominated by Cyperus spp. and E. pilosa, while the upland by Phyllanthus niruri. Furthermore, with the exception of βW, the WSB and diversity indices were found to be higher on the topsoil (0–15 cm). Our study establishes that the AFS system in the semi-arid sub-tropics has a more diverse WSB indicating a healthy system, as opposed to HCS, which has a dominance of certain weed species, opening the door for more severe infestation of invasive weed species.
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8

Dhatt, A. S. "PROSPECTS OF TEMPERATE FRUIT CULTIVATION IN INDO-GANGETIC PLAINS." Acta Horticulturae, no. 662 (December 2004): 107–9. http://dx.doi.org/10.17660/actahortic.2004.662.12.

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9

Saha, Pamela, and Devendra Singh. "Physcomitrium eurystomum (Bryophyta: Funariaceae) - An addition to Bryoflora of Central India." Indian Journal of Forestry 43, no. 4 (December 1, 2020): 341–44. http://dx.doi.org/10.54207/bsmps1000-2021-s04k5x.

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Physcomitrium eurystomum Sendtn. is recorded for the first time form Jharkhand, Central India, earlier known from West Himalayan, Western Ghats, Punjab and West Rajasthan and Gangetic Plains bryological territeries of India.
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10

Singh, S. "A new Rectolejeunea from Indian Botanic Garden, India." Indian Journal of Forestry 34, no. 3 (September 1, 2011): 341–44. http://dx.doi.org/10.54207/bsmps1000-2011-8l68j3.

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Rectolejeunea devendrae Sushil K.Singh, closely related to R. olivacea (Steph.) S.C. Srivast. and A. Agarwal, is described as a new species from Indian Botanic Garden, Howrah in Gangetic plains of West Bengal, India.
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11

Singh, Sushil. "A New Rectolejeunea from Indian Botanic Garden, India." Indian Journal of Forestry 35, no. 2 (June 1, 2012): 269–72. http://dx.doi.org/10.54207/bsmps1000-2012-59130v.

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Анотація:
Rectolejeunea devendrae Sushil K.Singh, closely related to R. olivacea (Steph.) S.C. Srivast. & A Agarwal, is described as a new species from Indian Botanic Garden, Howrah in Gangetic Plains of West Bengal, India.
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12

Ghude, Sachin D., G. S. Bhat, Thara Prabhakaran, R. K. Jenamani, D. M. Chate, P. D. Safai, A. K. Karipot, et al. "Winter Fog Experiment Over the Indo-Gangetic Plains of India." Current Science 112, no. 04 (February 1, 2017): 767. http://dx.doi.org/10.18520/cs/v112/i04/767-784.

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13

Adhikary, Pabitra. "Grassy weed management in aerobic rice in Indo-Gangetic plains." Indian Journal of Weed Science 48, no. 3 (2016): 262. http://dx.doi.org/10.5958/0974-8164.2016.00064.2.

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14

Jishnu, R. B., S. P. Naik, N. R. Patra, and J. N. Malik. "Ground response analysis of Kanpur soil along Indo-Gangetic Plains." Soil Dynamics and Earthquake Engineering 51 (August 2013): 47–57. http://dx.doi.org/10.1016/j.soildyn.2013.04.001.

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15

Mahajan, G., B. S. Chauhan, and D. E. Johnson. "Weed Management in Aerobic Rice in Northwestern Indo-Gangetic Plains." Journal of Crop Improvement 23, no. 4 (October 2009): 366–82. http://dx.doi.org/10.1080/15427520902970458.

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16

Sonkamble, Sahebrao, R. Rangarajan, R. Rajkumar, T. Warsi, T. Sambasivarao, and S. Ahmed. "Appraising Hydro-dynamics of Alluvial Aquifers from Indo-Gangetic Plains." Journal of the Geological Society of India 94, no. 5 (November 2019): 464–70. http://dx.doi.org/10.1007/s12594-019-1342-2.

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17

Park, Alex G., Adam S. Davis, and Andrew J. McDonald. "Priorities for wheat intensification in the Eastern Indo-Gangetic Plains." Global Food Security 17 (June 2018): 1–8. http://dx.doi.org/10.1016/j.gfs.2018.03.001.

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18

Kutty, Saumya Govindan, Ashok Priyadarshan Dimri, and Ismail Gultepe. "Climatic trends in fog occurrence over the Indo‐Gangetic plains." International Journal of Climatology 40, no. 4 (October 29, 2019): 2048–61. http://dx.doi.org/10.1002/joc.6317.

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19

SAWAISARJE, G. K., P. Khare, C. Y. SHIRKE, S. DEEPAKUMAR, and N. M. NARKHEDE. "Study of winter fog over Indian subcontinent : Climatological perspectives." MAUSAM 65, no. 1 (December 20, 2021): 19–28. http://dx.doi.org/10.54302/mausam.v65i1.858.

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Fog is localized phenomenon where horizontal visibility is reduced to less than 1000 m due to suspension of very small water droplets in the air. In fact Fog is cloud at surface level. This phenomenon matters to us in our daily activities due to its effect on life, public health, road safety, and economic prosperity. Its knowledge is essential to meet critical societal needs. In India, radiation and advection fog are most common which occur mostly over north India in winter. This study presents results of spatial variability of average number of days having visibility less than 1000 m at 0300 UTC during winter season over Indian subcontinent (0° N-35° N and 60° E-100° E) using synoptic hour daily surface data. Analysis of Fog events based on half hourly METAR observations for winter months (December 2010-February 2011) at selected ICAO stations of India is also presented. The monthly spatial variability of average number of days with fog having visibility less than 1000 m indicates presence of fog over Indo-Gangetic plains on an average of 7 to 10 days during December and more than 8 days during January. South Gangetic West Bengal is susceptible to fog during February. Seasonal variation of fog shows that there is prominence of fog over Indo-Gangetic plains on an average of more than 6.5 days. Significant incidences of foggy days occur over South Interior Karnataka and Coastal Karnataka has incidence of foggy days on an average of 6.5 days. North India is susceptible to dense fog on average of 2.5 days during the season while Gangetic West Bengal, West Rajasthan and adjoining parts of east Rajasthan and East Uttar Pradesh have occurrence of fog on an average of 3.5 days. Thick fog occurs on an average of 3 days over northern India during the winter season. Analysis of time series of air temperature, dew point temperature, dew point depression, visibility, zonal and meridional components of wind and its magnitude at selected ICAO stations indicate that visibility reduces to below 1000 m while light winds are southeasterly at Ahmedabad, northerly to northwesterly at Amritsar, northerly to northeasterly at New Delhi, westerly to southwesterly at Kolkata, Guwahati and dew point depression is below 3 °C during such conditions. Long period 1971-2010 analysis of visibility conditions less than 1000 m over Indian subcontinent shows Indo-Gangetic plains region to have average wind speed to be 0.6 m/s, air temperature in the range 9 °C to 15 °C during December-February at 0300 UTC. Long period 1971- 2010 analysis of relative humidity shows Indo-Genetic plains region to have relative humidity in the range 72% to 84% at 0300 UTC during December-February.
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20

Adhikarimayum, Aisho Sharma, and G. V. Gopi. "First photographic record of tiger presence at higher elevations of the Mishmi Hills in the Eastern Himalayan Biodiversity Hotspot, Arunachal Pradesh, India." Journal of Threatened Taxa 10, no. 13 (November 26, 2018): 12833–36. http://dx.doi.org/10.11609/jott.4381.10.13.12833-12836.

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India is home to 70% of the global Tiger Panthera tigris population, resident in five major areas: Shivalik Gangetic Plains, Central & Eastern Ghats, Western Ghats, the Sundarbans, and the northeastern Hills and Brahmaputra flood plain. Information about tiger ecology in temperate forests is limited. During January–May 2017, two male tigers were photo-captured in the Mishmi Hills at altitudes of 3,246m and 3630m, where vegetation ranges from temperate mixed forest to sub alpine forest. The landscape with newly-discovered tigers merits priority protection, and other likely tiger habitats in this region should be surveyed for their presence.
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21

Gandhi, Vasant P., and Nicky Johnson. "Enhancing Performance of Participatory Water Institutions in the Eastern Indo-Gangetic Plains: What Can We Learn from New Institutional Economics and Governance Theories?" Water 12, no. 1 (December 23, 2019): 70. http://dx.doi.org/10.3390/w12010070.

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The paper examines the performance of participatory water institutions in India’s Eastern Indo-Gangetic plains region using new institutional economics and management governance fundamentals. Water institutions are of great importance for water resource management in India’s Eastern Indo-Gangetic plains since the region has relatively abundant water but lags behind significantly in economic development and growth with a high incidence of poverty. Engineering solutions to water management have been implemented but have not given good results principally because of weak institutional development and design in the region. Effective and efficient participatory water institutions are urgently needed. The research uses concepts from new institutional economics and management governance theory to build a conceptual framework for explaining the performance of participatory water institutions. The framework identifies eight institutional rationalities: technical, environmental, economic, social, political organizational, financial and government; as well as five institutional features: clear objectives, good interaction, adaptiveness, right scale, and compliance, as linked to performance. Based on this, a survey instrument was developed and a survey conducted obtaining responses from more than 500 households across 51 such institutions in the eastern Indo-Gangetic plains states of Assam and Bihar. The data were analyzed through statistical and econometric techniques including Ordered-Probit. The results support the relevance of the concepts in explaining performance of water institutions, and a number of drivers of performance were identified through Ordered-Probit, particularly, four rationalities—technical, economic, social and organizational, (with coefficients (0.4622, 0.3803, 0.4303, 0.2457) and three institutional features—good interaction, adaptiveness and appropriate scale (with coefficients 0.4242, 0.2703, 0.6756) (based on a 5-point Likert scale), as playing a positive and significant role in enhancing performance. The results provide a number of useful insights which can help guide interventions and policy towards better design and development of the water institutions, and help improve water resource management and livelihoods in the region.
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22

Sinha, Rajiv, Peter F. Friend, and V. R. Switsur. "Radiocarbon dating and sedimentation rates in the Holocene alluvial sediments of the northern Bihar plains, India." Geological Magazine 133, no. 1 (January 1996): 85–90. http://dx.doi.org/10.1017/s0016756800007263.

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AbstractSeven radiocarbon dates of carbonate shells and charcoal from the upper two metres of sediment in the Indo-Gangetic plains of northern Bihar, eastern India, can be divided into three groups, with the following approximate ages: 2400±45 a BP (two samples), 1100±45 a BP (four samples) and 765±45 a BP (one sample). This evidence for at least three episodes of sedimentation in the last 2400 a contrasts with evidence of greater ages from similarly near-surface sediments in the middle Gangetic plains of Uttar Pradesh, further west. In these more westerly areas, greater ages and well-developed river terraces point to much more restricted late Holocene sedimentation. Rates of net sediment accumulation calculated using our Bihar ages, spanning a period of the order of 103–104 a, are similar to those calculated for periods of the order of 105–106 a for the Himalayan foreland basin. This suggests that, in the whole basin case, short-period rates higher than the Bihar rates have been compensated by longer than Bihar periods of non-deposition or erosion.
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23

Kumar, Arun, Lalit Kumar Rolaniya, Robin Kumar, and Kapil Kumar. "Conservation agriculture adoption and constrain in indo gangetic plains: An overview." Progressive Agriculture 18, no. 1 (2018): 48. http://dx.doi.org/10.5958/0976-4615.2018.00007.8.

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24

Kumar, Rakesh, and Rajkumar Jat. "Water requirements and irrigation scheduling of maize in Northern Gangetic plains." INTERNATIONAL JOURNAL OF AGRICULTURAL ENGINEERING 11, no. 1 (April 15, 2018): 210–15. http://dx.doi.org/10.15740/has/ijae/11.1/210-215.

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25

Gangopadhyay, Samar K., P. Chandran, S. K. Ray, and A. K. Maitra. "Genesis of soils of middle indo-gangetic plains of Bihar, India." Clay Research 40, no. 2 (2021): 88–99. http://dx.doi.org/10.5958/0974-4509.2021.00010.3.

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26

Gupta, Aashi. "Effects of Climate Change on Agricultural Patterns of Indo-Gangetic Plains." Asian Man (The) - An International Journal 15, no. 1 (2021): 92–99. http://dx.doi.org/10.5958/0975-6884.2021.00012.8.

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27

K. Singh, Anil, Dhananjay Kumar, Anjana Sisodia, and Minakshi Padhi. "Varietal Evaluation of Gladiolus for Flowering Attributes Under Indo-Gangetic Plains." International Journal of Current Microbiology and Applied Sciences 7, no. 07 (July 10, 2018): 3728–35. http://dx.doi.org/10.20546/ijcmas.2018.707.431.

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28

Biswas, Soumik, Bishal Mukherjee, Ammaruddin Munshi, Subrata Chongre, and Manabendra Ray. "Evaluation of Mustard Hybrid varieties in Gangetic Plains of West Bengal." International Journal of Current Microbiology and Applied Sciences 8, no. 10 (October 10, 2019): 585–90. http://dx.doi.org/10.20546/ijcmas.2019.810.065.

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29

Anbukkani, P., M. L. Nithyashree, and Pramod Kumar. "Productivity and Sustainability of Rice-Wheat System in Indo-Gangetic Plains." Indian Journal of Economics and Development 12, no. 3 (2016): 549. http://dx.doi.org/10.5958/2322-0430.2016.00173.6.

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30

Raghucharan, M. C., and Surendra Nadh Somala. "Seismic damage and loss estimation for central Indo-Gangetic Plains, India." Natural Hazards 94, no. 2 (August 18, 2018): 883–904. http://dx.doi.org/10.1007/s11069-018-3430-9.

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31

Kaskaoutis, D. G., E. E. Houssos, D. Goto, A. Bartzokas, P. T. Nastos, P. R. Sinha, S. K. Kharol, P. G. Kosmopoulos, R. P. Singh, and T. Takemura. "Synoptic weather conditions and aerosol episodes over Indo-Gangetic Plains, India." Climate Dynamics 43, no. 9-10 (January 25, 2014): 2313–31. http://dx.doi.org/10.1007/s00382-014-2055-2.

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32

Debnath, Subhankar, Ashok Mishra, D. R. Mailapalli, and N. S. Raghuwanshi. "Quantifying yield gap for rice cropping systems in Lower Gangetic Plains." Paddy and Water Environment 16, no. 3 (June 1, 2018): 601–15. http://dx.doi.org/10.1007/s10333-018-0653-z.

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33

BISWAS, B., and K. GUPTA. "Variability of southwest monsoon rainfall over West Bengal." MAUSAM 44, no. 4 (January 1, 2022): 353–58. http://dx.doi.org/10.54302/mausam.v44i4.3925.

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Анотація:
Monthly and seasonal variations of southwest monsoon rainfall over the districts of Gangetic and Sub-Himalayan West Bengal are presented and their differences discussed. Latitudinal variations of monsoon rainfall are brought out. Decadal means of seasonal rainfall over plains are compared with those at higher elevations and northern latitudes. An attempt is made to study long term rainfall trends.
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34

Bhargava, Devendra Swaroop. "Nature and the Ganga." Environmental Conservation 14, no. 4 (1987): 307–18. http://dx.doi.org/10.1017/s0376892900016829.

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The Ganga's unique and numerous virtues appear to be based on myths, but the reasons for its importance are traceable to scientific premises. The Ganga, symbolizing Indian culture and civilization, is regarded by the Hindus as the holiest amongst the rivers, and it is the Indo-Gangetic plain's most significant river owing to its mighty basin and course, and extraordinarily high self-purifying powers. The Ganga originates from Gangori in the Uttrakhand Himalayan glacier as an upland stream, emerges as a river of the plains at Rishikesh, and, after traversing almost the entirety of India from West to East, finally merges into the Bay of Bengal.
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35

Bais, Rajv K. Singh. "On the occurrence of Common Baron (Lepidoptera: Nymphalidae: Limenitidinae: Euthalia aconthea Cramer, 1777) in the Delhi area and analysis of abiotic factors affecting its distribution in India." Journal of Threatened Taxa 8, no. 12 (October 26, 2016): 9418. http://dx.doi.org/10.11609/jott.3112.8.12.9418-9433.

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This paper gives details of the occurrence of Euthalia aconthea from Delhi area situated in the Indo-Gangetic plains. Occurrence records of this species suggest that it is most frequent in five zones of India, despite the fact that its main larval food plant Mango Mangifera indica is abundantly available almost throughout India. Possible abiotic factors are hypothesized for this distribution.
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Prasad, Bipin Kishore, Abhijit Basu, and Ajay Kumar Rai. "A Study on Satisfaction Levels among Hearing Aid Users in Gangetic Plains." Bengal Journal of Otolaryngology and Head Neck Surgery 28, no. 3 (February 5, 2021): 203–8. http://dx.doi.org/10.47210/bjohns.2020.v28i3.286.

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Introduction Outcome assessments have emerged as an effective method for determining whether or not hearing aids are working to achieve positive results in rehabilitating the hearing impaired. Present study aims to assess the satisfaction level of clientele using hearing aids. Material and Methods One hundred and fourteen (114) hearing handicapped patients, fitted with government-provided hearing aids at various clinics spread over Gangetic plains were included in this prospective observational study for outcome analysis. Follow up was done at 2 weeks and 45 days when they were further motivated to continue using the aid, comfortable fitting of mould was ensured along with minor trouble shooting. Four and half months later, their satisfaction level was assessed by analysing their response to Clientele Satisfaction Questionnaire. Results Fifty percent of the patients were motivated by their family members to try the aid whereas 50% were self motivated. Better communication with family members and immediate social circle was the common motive. Majority (85%) reported high level of satisfaction in terms of hearing benefit. Patients with severe degree of hearing loss were more satisfied and used the aid for longer duration in a day. Handling the aid was not as much of a problem as tolerating the noise produced by aid itself. Cost of battery was a concern for 80% of our clientele. Conclusion Proper fitting of hearing aid improved the quality of life of majority of our hearing handicapped clientele by overcoming their psychosocial problems.
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Yaduvanshi, Aradhana, and Anand Kr Sinha. "Extreme event characterization for the river basins of Eastern Indian Gangetic Plains." Hydrology Research 49, no. 1 (March 3, 2017): 210–21. http://dx.doi.org/10.2166/nh.2017.211.

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Abstract The Eastern Indian Gangetic Plains are characterized by a primarily nature-dependent region blessed with an enormous supply of mineral resources. The region is witnessing a rapid transition in its demographic structure because of rapid industrialization. The region provides a classic example of an area which shows a trend reverse to that observed globally, as far as the frequency of extreme precipitation events is concerned. This paper provides a risk characterization of the entire region, based on the empirical behavior shown by data available so far, in addition to predictions based on theory of extreme values. The long-term behavior prediction is made with an aim to provide policy makers ample time and direction to develop suitable disaster prevention measures. The focus is primarily on extremely high rainfall events, their frequency, trend and estimated long-term behavior. The study corroborates the stability assumption behind the Indian monsoon, and also provides an indication of the expected long-term as well as short-term threats. This study provides a unique application of the extreme value theory to help in developing a threat map for a region whose population is known to be highly impacted by any significant deviations from a normal monsoon.
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Bhatt, B. P., V. K. Gupta, Lokendra Kumar, Indu Shekhar Singh, and Bikash Sarkar. "Euryale ferox (Salisb): Promising Aquatic Food Crop of Eastern Indo Gangetic Plains." International Journal of Current Microbiology and Applied Sciences 6, no. 6 (June 10, 2017): 1914–21. http://dx.doi.org/10.20546/ijcmas.2017.606.223.

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39

Rakesh Kumar , Sanjay Kumar, Rakesh Kumar ,. Sanjay Kumar. "Estimation of Solar Panel Power for Irrigated Crops in Northern Gangetic Plains." International Journal of Agricultural Science and Research 8, no. 1 (2018): 91–104. http://dx.doi.org/10.24247/ijasrfeb201814.

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40

Leder, Stephanie, Fraser Sugden, Manita Raut, Dhananjay Ray, and Panchali Saikia. "Ambivalences of collective farming: Feminist political ecologies from the Eastern Gangetic Plains." International Journal of the Commons 13, no. 1 (May 8, 2019): 105. http://dx.doi.org/10.18352/ijc.917.

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41

SINHA, RAJIV, and PETER F. FRIEND. "River systems and their sediment flux, Indo-Gangetic plains, Northern Bihar, India." Sedimentology 41, no. 4 (August 1994): 825–45. http://dx.doi.org/10.1111/j.1365-3091.1994.tb01426.x.

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42

Singh, Satvindar, B. Parkash, and Balaji Bhosle. "Pedogenic processes on the Ganga/Deoha-Ghaghara Interfluve, Upper Gangetic Plains, India." Quaternary International 159, no. 1 (January 2007): 57–73. http://dx.doi.org/10.1016/j.quaint.2006.08.012.

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43

Krishan, Gopal, Surjeet Singh, Anurag Khanna, R. P. Singh, and N. C. Ghosh. "Current Groundwater Conditions in Alluvial Gangetic Plains of Haridwar District, Uttarakhand, India." Current World Environment 11, no. 3 (December 25, 2016): 737–42. http://dx.doi.org/10.12944/cwe.11.3.07.

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In the present study, data of 41 hydrograph stations distributed in the Haridwar district are analysed for the years 2014-15 for depth to water level and water quality. The average depth to water level during pre-monsoon is found 10.74 m and in post-monsoon there is a rise of 0.23 m in average water level and found 10.51 m. Among all the 6 blocks viz. Bhagwanpur, Bhadarabad, Khanpur, Laksar, Narsan and Roorkee, the distribution of water level shows that the water levels are deep in the entire Bhagwanpur block. For assessing the groundwater quality, the water samples were collected from 40 sites covering the entire district. The groundwater is formed as Ca-Mg-HCO3 type. In the groundwater, alkaline earths exceed the alkalis and weak acids dominate strong acids. Although groundwater quality is good for drinking as well as irrigation purpose but in few samples higher concentrations of NO3-, Cl− and SO42− ions are found and hence continuous monitoring is required for these ions as precautionary measures.
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44

Krishna, Vijesh V., and Prakashan C. Veettil. "Productivity and efficiency impacts of conservation tillage in northwest Indo-Gangetic Plains." Agricultural Systems 127 (May 2014): 126–38. http://dx.doi.org/10.1016/j.agsy.2014.02.004.

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45

Chaudhary, V. P., B. Gangwar, D. K. Pandey, and K. S. Gangwar. "Energy auditing of diversified rice–wheat cropping systems in Indo-gangetic plains." Energy 34, no. 9 (September 2009): 1091–96. http://dx.doi.org/10.1016/j.energy.2009.04.017.

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46

Sinha, R., Vikrant Jain, G. Prasad Babu, and S. Ghosh. "Geomorphic characterization and diversity of the fluvial systems of the Gangetic Plains." Geomorphology 70, no. 3-4 (September 2005): 207–25. http://dx.doi.org/10.1016/j.geomorph.2005.02.006.

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47

Singh, Vimla, Shrvan Kumar, Madan Lal, and K. S. Hooda. "Cultural and morphological variability amongRhizoctonia solaniisolates from trans-gangetic plains of India." Research on Crops 15, no. 3 (2014): 644. http://dx.doi.org/10.5958/2348-7542.2014.01390.4.

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48

Das, Ruma, Rahul Kumar, Dibyendu Sarkar, Shrila Das, Amit Kumar Pradhan, Debarup Das, Manoj Srivastava, et al. "Boron fractions and its availability in soils of the Indo-Gangetic plains." CATENA 222 (March 2023): 106877. http://dx.doi.org/10.1016/j.catena.2022.106877.

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49

Singh, K. P., A. Malik, D. Mohan, and S. Sinha. "Persistent Organochlorine Pesticide Residues in Alluvial Groundwater Aquifers of Gangetic Plains, India." Bulletin of Environmental Contamination and Toxicology 74, no. 1 (January 2005): 162–69. http://dx.doi.org/10.1007/s00128-004-0563-1.

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50

PRASAD, A., S. SINGH, S. CHAUHAN, M. SRIVASTAVA, R. SINGH, and R. SINGH. "Aerosol radiative forcing over the Indo-Gangetic plains during major dust storms." Atmospheric Environment 41, no. 29 (September 2007): 6289–301. http://dx.doi.org/10.1016/j.atmosenv.2007.03.060.

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