| تعداد نشریات | 285 |
| تعداد نشریات سازمان | 83 |
| تعداد شمارهها | 3,094 |
| تعداد مقالات | 34,552 |
| تعداد مشاهده مقاله | 49,452,648 |
| تعداد دریافت فایل اصل مقاله | 79,880,303 |
تغییرات فصلی ذخیره کربن آلی خاک در توده مدیریتشده و مدیریتنشده راش- ممرز | ||
| تحقیقات جنگل و صنوبر ایران | ||
| مقاله 11، دوره 25، شماره 2 - شماره پیاپی 68، تیر 1396، صفحه 286-297 اصل مقاله (447.61 K) | ||
| نوع مقاله: علمی- پژوهشی | ||
| شناسه دیجیتال (DOI): 10.22092/ijfpr.2017.111768 | ||
| نویسندگان | ||
| مریم مصلحی1؛ هاشم حبشی* 2؛ رامین رحمانی2 | ||
| 1دکتری جنگلشناسی و اکولوژی جنگل، دانشکده علوم جنگل، دانشگاه علوم کشاورزی و منابع طبیعی گرگان، گرگان، ایران | ||
| 2دانشیار، گروه جنگلشناسی و اکولوژی جنگل، دانشکده علوم جنگل، دانشگاه علوم کشاورزی و منابع طبیعی گرگان، گرگان، ایران | ||
| چکیده | ||
| کربن آلی خاک یکی از مهمترین مؤلفههای چرخه جهانی کربن است، بنابراین خاک جنگلها بهعنوان یکی از بزرگترین ذخیرهگاههای کربن آلی در اکوسیستم خشکی در کنترل غلظت Co2 اتمسفر نقش اساسی دارد. دخالت در اکوسیستم جنگلی در مقطع زمانی نامناسب با تغییر در آزادسازی یا جذب کربن در آن، تأثیرات قابل ملاحظهای بر غلظت Co2 اتمسفر و گرمایش جهانی دارد. این پژوهش به بررسی تأثیر شیوه گزینشی بر تغییرات ذخیره کربن آلی خاک در فصول مختلف در تودههای آمیخته راش- ممرز سری یک طرح جنگلداری دکتر بهرامنیا استان گلستان پرداخت. تغییرات ذخیره کربن آلی خاک از بهمن 1392 بهمدت یکسال در چهار توده یک هکتاری (توده بکر پارسل 32 و پارسلهای 30، 33 و 31 که بهترتیب 10، هفت و یک سال از دخالت در آنها میگذشت) در عمق صفر تا 20 سانتیمتری بررسی شد. تغییرات درجه حرارت و رطوبت خاک بهعنوان عاملهای تأثیرگذار بر ذخیره کربن اندازهگیری شدند. برای تعیین تغییرات رطوبت و حرارت خاک در هریک از تیمارها از تجزیه واریانس یکطرفه و برای مقایسه فصلی ذخیره کربن آلی خاک در هر تیمار، از طرح اندازههای تکراری استفاده شد. رابطه ذخیره کربن با رطوبت و حرارت خاک با استفاده از ضریب همبستگی پیرسون بررسی شد. نتایج نشان داد که تغییرات ماهانه رطوبت و حرارت خاک در هر تیمار دارای اختلاف معنیداری بود. ذخیره کربن آلی خاک با حرارت و رطوبت خاک نیز همبستگی معنیداری را نشان داد. بررسی ذخیره کربن آلی خاک در فصول مختلف، اختلاف معنیداری را نشان داد، اما این اختلاف در تیمارهای مدیریتشده بیشتر مشهود بود. در تودههای مدیریتشده، ذخیره کربن در تابستان کاهش شدیدی نسبت به توده شاهد داشت. | ||
| کلیدواژهها | ||
| استان گلستان؛ درجه حرارت خاک؛ رطوبت خاک؛ شیوه گزینشی؛ طرح جنگلداری | ||
| عنوان مقاله [English] | ||
| Seasonal changes of soil organic carbon pool in the managed and unmanaged beech-hornbeam stands | ||
| نویسندگان [English] | ||
| Maryam Moslehi1؛ Hashem habashi2؛ Ramin Rahmani2 | ||
| 1Ph.D. Silviculture and Forest Ecology, Faculty of Forest Sciences, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran | ||
| 2Associate Prof., Department of Silviculture and Forest Ecology, Faculty of Forest Sciences, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran | ||
| چکیده [English] | ||
| Soil organic carbon (SOC) is a major component of global carbon cycle, hence forest soil as one of the major carbon sinks has a key role in the control of atmospheric Co2 concentrations. Consequently, changes of carbon release or uptake by forest ecosystems due to disturbance or management in an unsuitable period can have a considerable impact on atmospheric Co2 concentrations and global warming. In this study, the effect of selection systems were investigated on seasonal changes of soil organic carbon pool (SOCP) in the mixed beech-hornbeam stand in district one of Shastkolate forest, Golestan province. For this purpose, SOCP was determined in depth of 0-20 cm from February of 2014 to February of 2015 in four stands with one hectare area (one in compartment 32 of virgin forest) and three in compartments 30, 33 and 31 in managed forest, in which the last interventions date back to 10, 7 and 1 years ago). Soil temperature and moisture changes were measured through one year as effective factors on SOCP. One-way ANOVA were used to determine soil moisture and temperature variability in each treatment through one year, and seasonal dynamics of SOCP were comprised using repeated measures design (General linear model). The SOCP relationship with soil moisture and temperature were analyzed using Pearson correlation coefficient. Results showed that the monthly changes of soil moisture and temperature had a significant difference in each treatment. SOCP was also significantly correlated with soil moisture and temperature. SOCP difference in different seasons was also significant, which was more obvious in the managed treatments. SOCP showed severe decrease in the managed stands compared to the unmanaged stand in the summer. | ||
| کلیدواژهها [English] | ||
| Forest management plan, Golestan Province, Soil Moisture, Soil temperature, selection method | ||
| مراجع | ||
|
- Abd Latif, Z. and Blackburn, G.A., 2008. Forest microclimate modelling using gap and canopy properties derived from LiDAR and hyper spectral imagery. SilviLaser, 17: 151-158. - Anonymous, 2008. Forest management plan of Dr. Bahramnia (District no. 1). Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, 447p (In Persian). - Black, C.A., 1965. Methods of Soil Analysis: Part I. Physical and Mineralogical Properties. American Society of Agronomy, Madison, Wisconsin, USA, 770p. - Boerner, R.E.J., Brinkman, J.A. and Smith, A., 2005. Seasonal variations in enzyme activity and organic carbon in soil of a burned unburned hardwood forest. Soil Biology and Biochemistry, 37: 1419-1426. - Devi, N. and Yadava, P.S., 2006. Seasonal dynamics in soil microbial biomass C, N and P in a mixed oak forest ecosystem of Manipur, north-east India. Applied Soil Ecology, 31: 220-227. - Dixon, R.K., Brown, S., Houghton, R.A., Solomon, A.M., Trexler, M.C. and Wisniewski, J., 1994. Carbon pools and flux of global forest ecosystems. Science, 263: 185-190. - Gelman, V., Hulkkonen, V., Kantola, R., Nousianen, M., Nousianen, V., and Poku-Marboah, M., 2013. Impact of Forest Management Practices on Forest Carbon, Interdisciplinary Approach to Forests and Climate Change. University of Helsinky, Helsinky, 20p. - Ghorbani, S. and Rahmani, R., 2008. Estimating of interception loss, stem flow and through fall in a natural stand of oriental beech (Shastkolateh forest). Iranian Journal of Forest and Poplar Research, 16(4): 638-648 (In Persian). - Giardina, C.P., Ryan, M.G., Hubbard, R.M. and Binkley, D., 2001. Tree species and soil textural controls on carbon and nitrogen mineralization rates. Soil Science Society of American Journal, 65: 1272-1279. - Goulden, M.L., Munger, J.W., Fan, S.M., Daube, B.C. and Wofsy, S.C., 1996. Measurements of carbon sequestration by long-term eddy covariance: methods and a critical evaluation of accuracy. Global Change Biology, 2: 169-182. - Hart, S.C. and Perry, D.A., 1999. Transferring soils from high- to low-elevation forests increases nitrogen cycling rates: climate change implications. Global Change Biology, 5(1): 23-32. - Hobbie, S.E., Schimel, J.P., Trumbore, S. and Randerson, J.R., 2000. Controls over carbon storage and turnover in high-latitude soils. Global Change Biology, 6: 196-210. - Houghton, R.A., Skole, D.L. and Nober, C.A., 2000. Annual fluxes of carbon from deforestation and regrowth in the Brazilian Amazon. Nature, 403: 301-304. - Jian, Z., Sil Ong, W., Qingkui, W. and YanXin, L., 2009. Remove from marked records content and seasonal change in soil labile organic carbon under different forest cover. Chinese Journal of Eco-Agriculture, 17: 41-47. - Jobbagy, E.G. and Jackson, R.B., 2000. The vertical distribution of soil organic carbon and its relation to climate and vegetation. Ecological Applications, 10: 423-436. - Kirschbaum, M.U.F., 1995. The temperature dependence of soil organic matter decomposition and the effect of global warming on soil organic C storage. Soil Biology Biochemistry, 27(6): 753-760. - Lal, R., Kimble, J.M., Follet, R.F. and Cole, C.V., 1998. The Potential of U.S. Cropland to Sequester Carbon and Mitigate the Greenhouse Effect. Ann Arbor Science Publication, Chelsea, 108p. - Liddcoat, C., Schapel, A., Davenport, D. and Dwyer, E., 2010. Soil Carbon and Climate Change, Rural Solutions. PIRSA Discussion Paper. Adelaide. SA: Rural Solutions SA, 76p. - Malhi, Y., Baldocchi, D.D. and Jarvis, P.G., 1999. The carbon balance of tropical, temperate and boreal forests. Plant, Cell and Environment, 22: 715-740. - Page, A.L., Miller, R.H. and Keeney, M., 1992. Methods of Soil Analysis, Part II, Chemical and Microbiological Methods. 2nd Edition, Soil Science Society of America Publication, USA, 1159p. - Qi, G., Wang, Q., Zhou, W., Ding, H., Wang, X., Qi, L., Wang, Y., Li, S. and Dai, L., 2011. Moisture effect on carbon and nitrogen mineralization in topsoil of Changbai mountain northeast China. Journal of Forest Science, 57(8): 340-348. - Ritter, E., 2005. Litter decomposition and nitrogen mineralization in newly formed gap sin a Danish Beech (Fagus sylvatica) forest. Soil Biology and Biochemistry, 37(7): 1237-1247. - Rustad, L., Campbell, J., Marion, G., Norby, R., Mitchell, M., Hartley, A., Cornelissen, J. and Gurevitch, J., 2001. A meta-analysis of the response of soil respiration, net nitrogen mineralization, and aboveground plant growth to experimental ecosystem warming. Oecologia, 126(4): 543-562. - Salim, M., Kumar, P., Gupta, M.K. and Kumar, S., 2015. Effect of seasons on sequestrated organic carbon pool in the soils under different land uses of Jhilmil Jheel Wetland, Haridwar-Uttrakhand, India. International Journal of Scientific and Research Publications, 5(1): 1-8. - Schulp, C.J.E., Nabuurs, G., Veburg, P.H. and de Waal, R.W., 2008. Effect of tree species on carbon stocks in forest floor and mineral soil and implications for soil carbon inventories. Forest Ecology and Management, 256(3): 482-490. < | ||
|
آمار تعداد مشاهده مقاله: 976 تعداد دریافت فایل اصل مقاله: 742 |
||