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Journals
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Gupta, M. K.
- Soil Water Interaction under Different Tree Plantations
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Indian Forester, Vol 135, No 1 (2009), Pagination: 47-54Abstract
A study on soil water retention pattern under Chir (Pinus roxburghii), Khair (Acacia catechu), Eucalyptus (Eucalyptus hybrid) plantation and barren land was conducted in Mussoorie Forest Division (UK). Multivariate test showed that the mean soil retention changes across the different soil depth. The maximum amount of water was retained by the soils under Khair (356.90 to 879.40 k lit/ha) followed by Chir (286.73 to 913.13 k lit/ha), Eucalyptus (212.50 to 932.50 k lit/ha) and the least under barren land (116.27 to 824.03 k lit/ ha) during the different months of the year. Good amount of water can be retained by the soils under plantation even in the drier months of April (255.20 to 393.27 k lit/ha) to June (21.50 to 356.90 k lit/ha) as compared to barren land (116.27 to 221.0 k lit/ha). Even in the driest month of May, surface layer can hold 148.89 % and over all entire profile by 217.73 % more water under plantations as compared to barren land. In drier months, lower layers had higher retention as compared to upper layers. From July to September, soil profile retained maximum water because entire profile gets recharged due to rainfall.Keywords
Soil-water Interaction, Tree Plantations, Mussoorie Forest Division, Uttarakhand- Soil Characteristics in Relation to Vegetation and Parent Material under Different Forest Covers in Kempty forest Range, Uttarakhand
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Forest Range, Mussoorie, Uttarakhand
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Indian Forester, Vol 135, No 3 (2009), Pagination: 331-341Abstract
Soil characteristics in relation to Forest vegetation and parent material in Kempty range of Mussoorie Forest Division, Uttarakhand have been studied. The results show that geologically, the rocks of the study area are of pre-cambrian to early paleozoic in age with recent and subrecent deposits. The organic matter and available nitrogen contents in the surface horizons increased with increase in altitude. The increase in the clay content of B horizon may be due to in-situ weathering of minerals. From the clay content of different horizons, it is quite evident that movement of clay from A to B horizon has taken place in all the profiles. Due to clay illuviation and greater thickness of B horizon, soils from Sainj, Kempty and Mailgarh blocks having Pinus roxburghii, Quercus leucotrichophora and Dalbergia sissoo vegetation, respectively, appeared to be more developed than those from Kheragarh and Gandiyala blocks (Miscellaneous and barren land). Statistical analysis showed that source of variations in different soil characteristics are significant for Clay, pH, CEC, Ex. Na, Available N and WHC for replications It has been observed that Q. leucotrichophora and P. roxburghii forests occur in the soils of Mollisols order on limestone, dolomite, shale, slate and quartzite (Kempty and Sainj blocks) whereas presence of phyllite (Mailgarh and Kheragarh blocks) shale, sandstone, quartzite etc. resulted in Ultisols order. The barren land soil of Gandiyala block belonged to Mollisols order. Findings of the study will be helpful to formulate the strategies for sustainable management of the natural forests and to work out potential productivity of soil and forest etc. for the overall afforestation of such lands and to create deeper understanding of natural stands ensuring ecological and economic benefits reaching the rural masses.Keywords
Soil Characteristics, Parent Material, Vegetation, Different Forest Covers, KemptyForest Range, Mussoorie, Uttarakhand
- Site Evaluation of Different Plantations in Mussoorie forest Division Using Discriminant Analysis
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Indian Forester, Vol 130, No 2 (2004), Pagination: 165-172Abstract
Soil samples were collected from Langha Forest of Mussoorie Forest Division, Uttaranchal, India under five different plantations (Dalbergia sissoo, Pinus roxburghii, Eucalyptus hybrid, Tectona grandis and Acacia catechu) to classify them for species suitability for afforestation. The four discriminate functions together with functions of plantations were given. This analysis identified potential discriminators as Available N, Organic matter, Available K and Total K for discrimination of plantations.- Light Intensity Pattern Under Agroforestry System
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Indian Forester, Vol 129, No 5 (2003), Pagination: 564-570Abstract
A study was conducted in Saini Majra (Haryana) under agroforestry system and at nearby open area to investigate the light intensity pattern under both the sites. Open area received 96.42% higher light intensity as compared to agroforestry system because there were no trees on the field. Maximum light intensity was recorded during mid-day (1210 to 1235 hrs) under both the sites. It is evident from the study that Poplar trees planted in agroforestry system can absorb or reflect up to 51.76% solar radiation before reaching to the ground even at a leafless stage.- Soil Organic Carbon Store in Different Forests of India
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Indian Forester, Vol 129, No 6 (2003), Pagination: 714-724Abstract
Global warming and emission of CO2 are of world wide concern because these are creating environmental imbalance and are a long term threat to the well being of all life on earth. Soil is a major sink of carbon. 9815.95 million tonnes of Soil Organic Carbon (SOC) store was estimated in total forest soils (as per 1994 forest stands) under 19 species spread over 27 States and Union territories in India. Spruce forest soil has maximum SOC store (386.0 t/ha) while Khair has minimum (51.93 t/ha). In India , miscellaneous forests are spread over an area of 40.7316 million ha , and their soils have maximum SOC store (6469.80 million tonnes) while in Hollong forest with an area of 0.0068 million ha , soils have the least SOC store (0.82 million million tonnes). Among the Indian States , Arunachal Pradesh has maximum SOC store (1702.08 million tonnes) while Dadra&Nagar Haveli has minimum (2.42 million tonnes) SOC store. Arunachal Pradesh ranks first in India having 248.11 t/ha SOC store in the soils of the State. Soil conservation practices should be strengthened to conserve these natural resources so that carbon store may not deplete especially from hilly terrain.- Moisture Distribution Pattern in the Soil under Different Tree Plantations
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Indian Forester, Vol 127, No 4 (2001), Pagination: 443-449Abstract
Soil moisture distribution pattern in the soil profiles under Chir, Teak, Shisham, Eucalyptus, Khair plantations, natural Sal and barren land was studied. It is observed that maximum moisture was retained by the soil under Shisham followed by natural Sal, Khair, Chir, Eucalyptus, Teak and the least was under barren land. As far as months are concerned maximum moisture was observed in August followed by September, July, October, November, January, March, February, December, April, June and the least moisture was in May. It has been found that during January, February, July and August moisture content decreased with increasing soil depth while in remaining months moisture content increase with increasing soil depth.- Factor Analysis of Soil Nutrient Distribution Pattern under Different Plantations
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Indian Forester, Vol 126, No 12 (2000), Pagination: 1270-1278Abstract
Factor analysis of soil nutrient distribution pattern under Chir, Teak, Eucalyptus, Shish am and Khair, in Mussoorie Forest Division (U.P.) was studied. It was done to identify underlying factors that are responsible for correlation among nutrients under five plantations. Eigen values for the first four factors were > 0.90 and combined accounted for 77 percent of total variation in the soil supporting the five plantations. The four factor model explained > 90 percent of the variance in total phosphorus; 85 percent of the variance in organic matter and available nitrogen; and > 70 percent of the variance in total nitrogen, total potassium, and total sodium, available potassium and available phosphorus. However the four factor model explained only 62 percent of the variance in available potassium and 66 percent of the variance in total calcium. The four extracted factors are aggrading factor (36.6 percent), Sodium factor (16.16 percent), Phosphorus factor (12.67 percent) and total phosphorus factor (11.92 percent) obtain through varimax orthogonal factor analysis.- Soil Potassium Changes at Different Altitudes and Seasons in Upper Yamuna Forests of Garhwal Himalayas
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Indian Forester, Vol 132, No 5 (2006), Pagination: 609-614Abstract
A study was conducted in Yamuna Forest Division of Garhwal Himalayas to determine the potassium status in the soils of different altitudes and seasons, and establish their correlation. The results showed general decrease in potassium down the soil profile with respect to altitude and seasons but increased with higher altitude. The seasonal effect showed higher values in autumn than spring. Total and available potassium showed highly significant positive correlation at all the altitudes and seasons and significant negative correlation with soil depth. In general, the soils at different altitudes are well supplied with potassium.- Response of Organic and Chemical Fertilizers to the Establishment and Growth of Eucalyptus in Sodic Land of Uttar Pradesh, India
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Indian Forester, Vol 132, No 6 (2006), Pagination: 726-736Abstract
An experiment was, taken up to evaluate the relative efficiency of organic residues in the form of oil cakes and to compare the effect of chemical fertilizers and organic residues on the growth performance of Eucalyptus planted on sodic soil at Harkumau village in District Sultanpur of Eastern Uttar Pradesh (U.P.). Four oil cakes viz., Neem cake, Sunflower cake, Mahua cake and Mustard cake in different doses, along with FYM and chemical fertilizer were tested. When the effect of different organic cakes was compared with chemical fertilizer, maximum increase in height over chemical fertilizer treatment was observed in Neem cake 1.0 kg/pit (91.09 %) followed by Mustard cake 1.5 kg/pit treatment (82.57 %). However, the maximum increase in collar diameter over chemical fertilizers, was shown by Mustard cake 1.5 kg/pit treatment (674.49 %) followed by Neem cake 1.0 kg/pit treatment (368.72 %). In comparison to chemical fertilizer, the Neem cake 1.0 kg/pit treatment caused better survival (34.30 %) followed by Mahua cake 1.5 kg/pit treatment (32.76 %).- Carbon Sequestration through Soil Organic Carbon Pool under Different forests Covers in Chamoli District of Uttarakhand
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Indian Forester, Vol 138, No 3 (2012), Pagination: 207-211Abstract
A study was conducted to estimate soil organic carbon pool (SOC) in three land uses viz. forests, horticulture and grassland in Chamoli district. Under forests land use, soil organic carbon pool was estimated in deodar (Cedrus deodara), quercus (Quercus leucotrichophora), chir (Pinus roxburghii), silver fir and spruce (Abies pindrow and Picea smithiana) and miscellaneous forests. Under horticulture land use SOC was estimated in mango orchards and under grass land SOC was estimated. Soil organic carbon pool under deodar was maximum (121.81 t ha-1) followed by Silver fir and Spruce (113.05 t ha1), Quercus (105.52 t ha-1), Chir (56.73 t ha-1) and the least was under miscellaneous (52.48 t ha-1). Forests of Chamoli district have 3,75,98,188.32 tones (37.59 million tons) and horticulture land use have 0.83 million tones, SOC pool in the soils. SOC pool under forests, grassland and horticulture were compared through ANOVA, SOC pool between forests, grassland and horticultures, were statistically significant different.Keywords
Soil Organic Carbon Pool, Climate Change, Forest Land Use, Horticulture, Grassland- Soil Moisture Accretion with Progressive Rainfall Under Tectona Grandis (Teak) and Eucalyptus Plantations
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Indian Forester, Vol 125, No 4 (1999), Pagination: 392-400Abstract
Gradual accretion of soil moisture in different depths with the progression of rainfall under Tectona grandis and Eucalyptus plantation at Langha range of Mussoorie Forest Division was studied. When cumulative rainfall rises upto 148.4 mm, water percolates only upto 75 cm depth under both plantation. At CRF 815.2 mm entire profile gets charged and no further increase in soil moisture was observed at 1421.1 m CRF, especially under Tectona grandis. The moisture accretion, in general, was higher in the soils supporting Eucalyptus in comparison to those under Teak plantation and, in particular in the lower depths at and above CRF of 815.2 mm. It was observed that during dry months soil moisture has positive relationship with depth.- Soil Organic Matter Status Under Different Social Forestry Plantations
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Indian Forester, Vol 125, No 9 (1999), Pagination: 883-890Abstract
A study was conducted in Langha Forest Range of Mussoorie Forest Division under 15 years old plantations of Pinus roxburghii, Tectona grandis, Dalbergia sissoo, Eucalyptus, Acacia catechu along with natural Shorea robusta forest and barren land to find out the status of soil organic matter. This study was conducted before and after monsoon to investigate the changes in SOM due to change of seasons. Before monsoon it was observed that SOM content was higher under natural Shorea robusta followed by Dalbergia sissoo, Eucalyptus, Tectona grandis, Acacia catechu and Pinus roxburghii plantations and least under barren land and after monsoon it was higher under Eucalyptus only in top (0-10 cm) layer but over all higher under the soils of natural Shorea robusta followed by Eucalyptus, Dalbergia sissoo, Pinus roxburghii, Acacia catechu, Tectona grandis and least under barren land. In general SOM was observed higher in post-monsoon in comparison to pre- monsoon period.- Soil Nutrient Changes Under Different Ages Eucalyptus Monocultures
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Indian Forester, Vol 122, No 1 (1996), Pagination: 55-60Abstract
Soil nutrient changes were studied under 5, 10, 15 and 20 years old Eucalyptus monocultures, in comparison to natural sal forest. Soil nutrient depletion under 10 and 15 years old monocultures were higher than 5 and 20 years old monocultures, in comparison to natural sal. Soil profile distribution of attribtttes showed gain in clay content and available P and loss in total K and P in all monocultures as compared to natural sal. The soil under 5 year and 20 year monocultures were less depleted because of faster mineralisation of residual organic matter in 5 years old monoculture and a gradation of soil nutrients as the monoculture aged as in 20 years old monoculture.- Studies on Soil Water Stable Aggregates in Silver Fir and Spruce Forests Managed under Diffeuent Silvicultural Systems in Himachal Pradesh
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Indian Forester, Vol 121, No 5 (1995), Pagination: 371-376Abstract
A study was carried out in Himachal Pradesh to investigate the water stable aggregate in silver fir and spruce forests under selection, shelterwood systems and clearfelled areas. Macro-aggregate (2-5 mm) and micro (0.10-0.5 mm) aggregates were more pronounced under selection system due to the higher organic matter and clay followed by shelterwood and clearfelled area. Macro-aggregates were higher in top layers while micro-aggregates were higher in lower layers in all sites.- Vegetation Survey and Ecological Studies under Silver Fir and Spruce Forests of Himachal Pradesh
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Indian Forester, Vol 118, No 7 (1992), Pagination: 460-465Abstract
This paper describes the phytosociological studies under spruce-fir (Picea smithiana and Ahies pindrow) forests at Narkanda, Himachal Pradesh. Abundance, frequency, density, Importance Value Index (I.V.I.) and morphological characters such as diameter, height and basal area have been worked out for individual ground vegetation species. The community is dominated by Fragaria indica and the contribution of Swertia chirata is recorded least in community development.- Autecology of Ailanthus glandulosa Desf. in Western Himalayas
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Indian Forester, Vol 118, No 12 (1992), Pagination: 917-921Abstract
The autecology or Ailanthus glandulosa Desf. in Western Himalayas was studied. Its biflmass and ischolar_main development was analysed. It is a good soil binding tree species and reproduces through seed and ischolar_main suckers. Seed remains viable for over one year.- Erodibility Status of Different Forest Soils in Himachal Pradesh
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Indian Forester, Vol 117, No 6 (1991), Pagination: 476-484Abstract
The Present Investigation Deals with Tbe Erosional Behaviour of Soils under Different Types of Land Use and forest Cover in Shimla, Bilaspur, Dharamsala and Nurpur forest Divisions of Himachal Pradesh. Suspension Percentage, Clay-moisture Equivalent Ratio, Dispersion and Erosion Ratio and Erosion Index have been Worked Out. Dispersion and Erosion Ratio and Suspension Percentage are Considered the most Elfective Indices of Soil Erodibility in the Present Study. On the Basis of Soil Studies, the Surface Soil of all the Areas is Affected by Sheet Erosion. The Erodibility Status of the Soils under Different Types of Land Uses have been Worked out in the Order: Scrub forest Soil > Orchard Soil > Burned forest Soli > forest Soil.- Studies on Root Behaviour, Biomass and Morphological Characters of Indigofera gerardiana Wall. In Western Himalayas
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Indian Forester, Vol 116, No 7 (1990), Pagination: 584-588Abstract
Indigofera gerardiana Wall, attains an average height of 1.37 m with 3.66 m2 average crown area. This shrub provides effective soil cover. Stem contributes maximum (53.8%) to the total biomass followed by ischolar_main (35.6%) and leaves (10.4%). Roots of a single plant can bind soil upto 1.34 m2 with the strong tap and lateral ischolar_mains. The taper rate varies from 0.19 to 0.25 in tap ischolar_main and 0.08 to 0.15 in lateral ischolar_mains which itself is an indication of strong ischolar_main system.- A Note, on Biomass and Root Characteristics of Artemisia maritima Linn.
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Indian Forester, Vol 116, No 8 (1990), Pagination: 674-675Abstract
No abstract- Studies on Biomass and Morphological Characters of Impatiens thomsoni Hook
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Indian Forester, Vol 116, No 9 (1990), Pagination: 757-758Abstract
No abstract- Soil and Vegetation Study of Lahaul and Spiti Cold Desert of Western Himalayas
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Indian Forester, Vol 116, No 10 (1990), Pagination: 785-790Abstract
Soil properties and vegetation studied in different localities of Labaul and Spiti valley of Western Himalayas are briefly described. The soil is silty clay loam, silty loam in texture having more alkalinity. Organic matter content varies from 0.08 to 2.98 per cent in the soil samples collected from different localities in the area under study. The nutrients e.g. Ca, K, Na and P were observed in decreasing order in all the sites. The growth of tree species, grasses and shrubs is poor because of the short growing period which is hardly five to six months or sometimes even less. Frequency, density, abundance, relative density and Importance Value Index (I.V.I.) bave been determined for each species. Hippophae rhamnoides is an important shrub used as fuelwood and as protective hedge. Important tree species of this valley bave also been described.- Soil Chemical Properties of Silver Fir and Spruce forests under Different Systems of Silviculture.
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Indian Forester, Vol 116, No 11 (1990), Pagination: 883-889Abstract
To study the effects of different management practices I e. selection, shelterwood and clearfelled on the status of soil potassium (total and available). An investigation has been carried out in silver fir (Abies pindrow) and spruce (Picea smithicna) forest of Narkada under Kumarsein Forest Range of H.P. Soils of this region were found sufficently rich in soil potassium contents with specific effects of management systems and site conditions clearly marked. Soil potassium decreased with increasing soil depth in all sites and management systems Intercorrelation between total and available potassium form was observed to be significantly positive. Soils of selection management system showed higher content of soil potassium followed by shelterwood and clearfelled systems, Same trend was observed in good, average and poor sites.- Studies on Biomass, Fodder Value, Coppicing Ability and Energy Contents of Debregeasia hypoleuca Wedd. in Western Himalayas
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Indian Forester, Vol 116, No 12 (1990), Pagination: 946-952Abstract
The present paper deals with the biomass of different plant parts, leaf fodder production. Coppicing effect and energy status of hypoleuca plants grown in nursery and under wild conditions. Emphasis has heen given on the need of fuelwood requirement of a family having five family members and its mitigation through the wood production of D hypoleuca. D hypoleu a coppiced well and the yield of branch wood, after coppicing, increased with increasing collar diameter. A farmer can grow D. hypoleuca easily on bis field boundaries or on terraces to fulfill his fodder, fuel and ropes requirements.- Soil Chemical Properties of Silver Fir and Spruce Forest Under Different Systems of Silviculture. I-Changes in Soil Nitrogen
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Fertility, Silver Fir, Spruce
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Indian Forester, Vol 115, No 4 (1989), Pagination: 235-242Abstract
Silvicultural management practices have differential impact on soil properties according to the system followed. An investigation was carried out in Picea smithiana and Abies pindrow forests managed under selection, shelterwood and clearfelled systems in Kotgarh Forest Division (H.P.) to quantify the differences in soil nitrogen status at different sites in the three management systems. Inter-correlation between total and available nitrogen, correlation of nitrogen status with soil depth in all the conditions have been reported Soils under selection system showed higher nitrogen accumulation followed by shelterwood and clearfelled systems. Soil nitrogen showed significant negative correlation with depth in all sites and management systems. A vailable and total nitrogen showed significant positive correlation in all sites and management systems.Keywords
Conifer Forests, Silvicultural Management, Soil Fertility, Soil Nitrogen, SiteFertility, Silver Fir, Spruce
- Infiltration Studies Under Different Forestry Management Systems in Western Himalayas
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Indian Forester, Vol 115, No 10 (1989), Pagination: 706-713Abstract
The present study reveals that selection system soil has more infiltration capacity than that under clearfelling system. Selection system provides longer opportunities for infiltration in comparison to clearfelled system due to more organic matter (6.72%) which increased porosity (56.7%) and water holding capacity (71.3%) of the forest soil. Clearfelling system provides less organic matter (4.62%) to the soil hence porosity (41.2%) and water bolding capacity (46.4%) of tree-less soils are comparatively lower.- Soil Chemical Properties of Silver Fir and Spruce Forest Under Different Systems of Silviculture. II-Changes in Soil Phosphorus
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Indian Forester, Vol 115, No 11 (1989), Pagination: 802-810Abstract
A study was conducted in Picea smithiana (Spruce) and Abies pindrow (Silver fir) forests managed under selection, shelterwood and clearfelled management systems in Kotgarh Forest Division (H.P.) to study the phosphorus behaviour in soils with challge in these systems. Level of soil phosphorus in different sites within the management systems, specific effects of management systems and site conditions. correlation between phosphorus level and soil depth in all conditions of the study, intercorrdation between total and available phospborus were worked out. Soils under selection system were well supplied with phosphorus followed by shelrerwoott and clearfelled systms. In many cases phosphorus level was indfpendent of soil depths as well as total and available forms were also mutually indeptendent of each other. The immobility of the element, biologically mediated uptake, soil pH etc. seemed to have brought about the pattern observed in this study The selection management and good site conditions have maintained better pbosphorus supply. Overall observations clearly indicate low soil phospborus supply in these forests.- Preliminary Studies on Methodology of Measuring the light Pattern Beneath the Canopy of Pinus roxburghii Plantation in Western Himalayas
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Indian Forester, Vol 114, No 8 (1988), Pagination: 462-469Abstract
The present investigation deals with the preliminary studies on methodology of measuring and quantification of light beneath the canopy of P. roxburghii plantation in Western Himalayas.- Effect of Pinus roxburghii Plantations on the Yield and Composition of Grasses in Temperate Region
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Indian Forester, Vol 111, No 10 (1985), Pagination: 787-793Abstract
Study on grass yield and composition under two age group plantations of Pinus roxburghii and open grassland was conducted at Kyarighat, 23 km from Shimla on Shimla-Kalka road during the year 1979, 1980 and 1981 respectively. Abundance, frequency, density and I.V.I. (Improtance Value Index) of each grass species under three sites have been recorded. Maximum yield (5094.36 kg/ha/yr) has been recorded in open grassland followed by Pinus roxburghii plantations of the year 1971 (4067.23 kg /ha/yr) and the year 1953 (3415.50 kg /ha/yr) respectively in decreasing order.- Litter Proouction and Release of Nutrients in Coniferous Forests of Himachal Pradesh
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Indian Forester, Vol 110, No 10 (1984), Pagination: 1014-1022Abstract
The present investigation deals with the litter production and nutrient tnrnover in four prominent coniferous species viz. Abies pindrow; Piceo smithiana; Cedrus deodara and Pinus wallichiano of Himachal Pradesh. Annual litter production and the amounts of nutrients released annually through litter fall bave been worked out in all the four species. A comparative account of nutrients released anually through litter fall lu different species is also prepared.- Interception Studies in Cedrus deodara Loudon Plantation in Himachal Pradesh
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Indian Forester, Vol 109, No 5 (1983), Pagination: 261-266Abstract
The present investigations deal with the throughfall, stemflow and intercreption loss in Cedius deodara Loudon plantation (94.5% crown density) or about 35 years age at Shillaroo, Kolgarh Forest Division, Distt. Simla (Himachal Pradesh). Of the total rainfall (1850.1 mm) 2.9% (55.3 mm) stemflow, 71.8% (1328.5 mm) throughfall and 25.2% (466.2 mm) interception loss were recorded respectively by for the whole study period. The minimum interception loss (18.7%) was observed in the month of July, 1980 which had the maximum (370.2 mm) rainfall. The highest interception (69.1%) was recorded in the month of February, 1980. which had the lowest (7.0 mm) rainfall. Interception loss was decreased with the increasing amount of precipitation.- Comparative Study of Infiltration in Soils under Forest Cover and Agriculture in Temperate Climate
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Indian Forester, Vol 108, No 10 (1982), Pagination: 648-652Abstract
Under both the condition of this study, the forest land has higher initial infiltration rates of 46.8 cm/hr and 5 cm/hr and final infiltration rates of .1 cm/hr in 150 mts and .1 cm/hr in 120 mts from forest areas as compared to .1 cm/hr in 60 mts ond 0 cm/hr in 20 mts from agricultural land after snow removal and snow melt respectively, due to thick layer of humus(10 cm) beneath the forest cover; higher organic matter (7.27%), higher moisture equivalent (29.87%), higher pore space (61.60%) and hIgher water balding capacity (60.26%) forest soils hafe resulted in higher infiltration rates in comparison to the agritultural soils, with no humus, low organic matter content (2.68%), lower moistnre equivalent (29.8%), lesser pore space (56.6%) and lower water holding capacity (46.88%).- Soil Organic Carbon Pool Under Different Land Uses in Haridwar District of Uttarakhand
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Indian Forester, Vol 137, No 1 (2011), Pagination: 105-112Abstract
Soil organic carbon was estimated in four land uses viz. forests, plantations, agroforestry and horticulture in Haridwar district. Over all 425 soil samples were collected from different land uses at various locations. Soil organic carbon, bulk density and coarse fragments were estimated in collected samples and SOC pool was calculated by using the equation as suggested by IPCC Good Practice Guidance for LULUCF. Maximum SOC pool (73.63 t/ha) was estimated under sal forest followed by miscellaneous forest (56.48 t/ha). Under horticulture land use, SOC pool was higher (58.66 t/ha) in the soils under litchi orchard as compared to Mango orchard (40.62 t/ha) and Guava (29.46 t/ha) orchard. Under block plantation, maximum SOC pool was estimated in the soils under teak (52.50 t/ha) followed by eucalyptus (39.06 t/ha), poplar (30.45 t/ha) and the least was under shisham (28.12 t/ha). Under agroforestry model, poplar - sugarcane showed higher SOC pool (25.78 t/ha) as compared to poplar - wheat (22.93 t/ha). On an average, Haridwar's forests have 65.05 t/ha SOC pool while horticultural land use have 42.91 t/ha, plantation have 37.53 t/ha and agro-forestry have 24.35 t/ha. Soils under forests stand show higher carbon pool than other land uses. Average SOC pool under forests was 65.05 t/ha, therefore, Haridwar district has 4.09 million ton of SOC pool under forests.Keywords
Soil Organic Carbon, Haridwar District, Sal, Mango, Guava, Eucalyptus, Poplar, Shisham- Soil Organic Carbon Store under Different Land Use Systems in Giri Catchment of Himachal Pradesh
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Indian Forester, Vol 136, No 9 (2010), Pagination: 1147-1154Abstract
Soil samples for the estimation of organic carbon store were collected from the entire catchment area starting from Rajban to origin of Giri and all the land uses were covered to estimate soil organic carbon. Soil organic carbon store in Giri catchment was estimated (up to the depth of 30 cm), and observed that maximum SOC store (93.47 t ha-1 ) was in the soils under Kail + Silver fir and Spruce forests and Kail + Quercus forests followed by Deodar forests (82.14 t ha-1). Soil organic carbon store under miscellaneous forests (57.66 t ha-1) and chir forests (57.33 t ha-1 ) was similar and the least SOC store was under sal forests (47.29 t/ha). Under agriculture land use, in cropping srstem soil organic store was 53.62 t ha-1 while under orchards it was 53.96 t ha-1. Altitude wise maxImum soil organic carbon pool was in the soils located above the altitude of 2500 m (91.37 t ha-1 ) followed by 2000-2500 m ( 88.68 t ha-1). The least SOC store was in the soils located below 1000 m (54.34 t ha-1). Girl catchment has 8,165,593.15 tones (8.16 million tons) soil organic carbon store in the forest area and under agriculture land use soil organic carbon store is 3,167,521.58 tones (3.16 million tons).Keywords
Carbon Sequestration, Soil Organic Carbon Estimation, Girl Catchment, Himachal Pradesh- Status of Sequestered Organic Carbon in the Soils under Different Vegetation Covers
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Indian Forester, Vol 139, No 7 (2013), Pagination: 571-575Abstract
Estimation of SOC pool under different vegetation covers was conducted in Almora district of Uttarakhand state in two land uses viz. forests where soil organic carbon pool was estimated in Deodar (Cedrus deodara), Quercus (Quercus leucotrichophora), Sal (Shorea robusta), Chir (Pinus roxburghii) and miscellaneous forests and under horticulture land use where SOC pool was estimated in apple orchards. Maximum SOC pool was observed in the soils under Deodar forest (114.36 t ha-1) followed by Quercus (91.77 t ha-1), Sal (61.51 t ha-1), Chir (54. 18 t ha-1) and the least was under miscellaneous (24.68 t ha-1). Subset for α= 0.05 indicate that Deodar stands separately (a), Quercus stand separately (b) Sal and Chir were together (c) and miscellaneous forest was also in separate SOC pool (d). SOC pool in soils under apple orchards was 61.99 t ha-1 . On an average, forests in Almora district have 73.76 t ha-1 SOC pool in the soils. All the forests of the districts have 1,74,20,939.95 tones (17.42 million tons) SOC store in the soils. In the district 1.26 million tons SOC pool was estimated in the soils under horticulture land use system.Keywords
Soil Organic Carbon Pool, Mitigation Potential, Forests, Horticulture- Soil Organic Carbon Status of Indian forests
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Affiliations
1 Indian Institute of Remote Sensing, Dehradun, IN
1 Indian Institute of Remote Sensing, Dehradun, IN
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Indian Forester, Vol 140, No 5 (2014), Pagination: 468-477Abstract
Soil organic carbon (SOC) is a major component of global carbon sinks and forests being one of the most important ecosystems for storing SOC. A database of SOC estimates along with other attribute information for different forest types of India were compiled from various literature sources and normalized for 1990 using modeling approach. Different thematic maps in digital format were prepared and harmonized using standard geospatial reference. The database was linked to thematic maps and used to estimate SOC densities and stock for three depth classes (0-25, 0-50 and 0-100 cm) in geographical information system. The mean soil organic carbon density estimates for top 30 cm ranged from 22.42 t/ha in sub-tropical dry evergreen forest to 100.33 t/ha in Himalayan moist temperate forest and similar trend was observed for top 0-50 and 0-100 cm as well. Soil organic carbon stock estimates for top 30 cm ranged from 1.89 Tg C in Himalayan dry temperate to 1406.68 Tg C in tropical moist deciduous forest and comparable trend was observed for top 0-50 and 0-100 cm. The total soil organic C pools in Indian forests have been estimated as 3.72, 5.25 and 7.66 Pg C in top 0-25, 0-50 and 0-100 cm soil depth respectively (1 Pg = 1000 Tg). The present database may form inputs in models to study carbon flux and help in prioritizing areas for carbon sequestration in Indian forests.Keywords
Soil Organic Carbon (soc), Indian Forests, Carbon Flux, Carbon Sequestration- Sequestered Organic Carbon Stock in the Soils under Different Land Uses in Western Region of Haryana
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Affiliations
1 Forest Soil and Land Reclamation Division, Forest Research Institute, P.O. New Forest, Dehradun-248 006 (Uttarakhand), IN
2 Forest Informatics Division, Forest Research Institute, Dehradun, IN
1 Forest Soil and Land Reclamation Division, Forest Research Institute, P.O. New Forest, Dehradun-248 006 (Uttarakhand), IN
2 Forest Informatics Division, Forest Research Institute, Dehradun, IN
Source
Indian Forester, Vol 141, No 7 (2015), Pagination: 718-725Abstract
A study was undertaken in western region Haryana comprising Bhiwani, Fatehabad, Hisar, Jind and Sirsa districts to estimate soil organic carbon stock under different land uses viz. forests, block plantations, horticulture, agroforestry and agriculture. Maximum organic carbon stock was found in the soils under forests (40.26 Mg ha-1). It was followed by plantation (33.27 Mg ha-1), horticulture (25.69 Mg ha-1), agroforestry (21.98 Mg ha-1) and the least SOC stock was under agriculture (18.10 Mg ha-1). Total soil organic carbon stock under forests was 1.22 million tons, out of these, Jind district has the maximum SOC stock (3, 17, 898.62 Mg). Least SOC stock was in Fatehabad district (1, 16, 086.27 Mg). Total SOC stocks under horticulture was 5, 23, 476.12 Mg, out of this, Sirsa district has 2, 64, 919.95 Mg and the least SOC stock was in Jind district (36,537.21 Mg). Soil organic carbon stock in Abubshehar Wildlife Sanctuary was 47, 7578.17 Mg and in Bir Bara Van Conservation Reserve was 19,490.85 Mg.Keywords
Soil Organic Carbon Stock, Western Region of Haryana, Forests, Plantations, Agroforestry, Horticulture, Agriculture.- Soil Organic Carbon Stocks Under Different Forest Types in India
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Affiliations
1 Biodiversity and Climate Change Division, Directorate of Research Indian Council of Forestry Research and Education, P.O. New Forest, Dehradun - Uttarakhand, IN
1 Biodiversity and Climate Change Division, Directorate of Research Indian Council of Forestry Research and Education, P.O. New Forest, Dehradun - Uttarakhand, IN
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Indian Forester, Vol 142, No 3 (2016), Pagination: 207-212Abstract
India has stabilized its forest and tree cover which is about 24.01 per cent of its total geographical area. Forests store significant amounts of carbon in its biomass, litter, dead woods and soil; and it has a major role in climate change adaptation and mitigation. Soil carbon is the largest terrestrial carbon pool and it holds a very important role in the carbon cycle. Soil samples were collected from all major forest types in different parts of the country as well as from adjoining non-forest areas for estimating the loss of soil organic carbon due to land conversion. The results of this study indicated that maximum soil organic carbon stock was under tropical moist deciduous forests (1665.65 million tonnes) followed by tropical dry deciduous forests (1572.38 million tonnes) and least under Himalayan dry temperate forests (3.85 million tonnes). The total soil organic carbon stocks i.e., 4327.36 million tonnes and 4680.25 million tonnes were estimated under the forests in the year 1995 and 2007 respectively. The estimate showed that due to increase in forest cover during the assessment period, soil in Indian forests acted as a net sink of 352.89 million tonnes of soil organic carbon. The maximum increase in soil organic carbon stock during this period was under tropical moist deciduous forests (125.91 million tonnes) and the least increase was under Himalayan dry temperate forests (0.23 million tonnes).Keywords
Soil Organic Carbon Stock, Forests, Forest Types, India.- Litter Fall, Nutrient Return and Soil Fertility Under Grewia optiva: An Indigenous Agroforestry Tree Species in Himachal Pradesh
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Affiliations
1 Forest Soil and Land Reclamation Division, Forest Research Institute, Dehradun 248 006, IN
1 Forest Soil and Land Reclamation Division, Forest Research Institute, Dehradun 248 006, IN