徒步活动对Bolu-Aladag冷杉林土壤某些物理性质的影响

A. Duyar, S. Kiniş
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The results of the measurement and evaluation; determined that Olu Ortu Kalinligi was decreased (r = 0.568**), and densitys of fresh soil (r = 0.440**) and dried soil (r = 0.423**) were increased in the trekking area. However, the effect on the soil Toprak Nemi was not observed. Based on the con trol field compared to the trampled area the average a 14% a Sikisma has occurred in the soil. During the trekking, the occurring of physical effects in the soil caused to compress on the litter and soil. Therefore, the soil infiltration capacity will reduce, then it may lead to being wildness and erosion. Keywords:  Litter, soil density, soil penetration Bolu-Aladag goknar ormanlarinda doga yuruyusu faaliyetlerinin topragin bazi fiziksel ozelliklerine etkisi Ozet:  Bu calisma, Bolu Aladag goknar ormanlarinda, doga yuruyuslerinin topraga etkisini arastirmak icin yapilmistir. Calismada 100 kisi olcum alanindan tek sira halinde yurumustur. Bu doga yuruyusunun olu ortu kalinligi, toprak yogunlugu, toprak nemi vb fiziksel ozelliklere etkisi incelenmistir. Calisma iki yil pes pese, iki ayri parselde ve ucer tekerrurlu olarak yapilmistir. Olu ortu kalinligi (cm), miktari (gr/m2) olarak belirlenmistir. Taze ve kurutulmus toprak yogunluklari (g/l) hacim silindirleri kullanilarak, toprak nemi (%) de taze ve kuru agirlik farkindan yararlanilarak belirlenmistir. Yapilan olcumler ve degerlendirmelerin sonucunda; doga yuruyusu yapilan alanda olu ortu kalinliginin azaldigi (r=0,568**), taze (r=0,440**) ve kurutulmus (r=0,423**) toprak yogunlugunda artisa neden oldugu belirlenmistir. Ancak toprak nemi uzerinde etkisi gorulmemistir. Kontrol alanina gore kiyaslandiginda cignenilen alan  topraginda ortalama %14 oraninda sikisma meydana geldigi bulunmustur. Doga yuruyusu esnasinda cignenen toprakta meydana fiziksel etkiler olu ortude ve toprakta sikismaya neden olmustur. Dolayisiyla topragin gecirgenlik kapasitesini dusurecek, devaminda yabanlasmaya ve erozyona yol acabilecektir. Anahtar Kelimeler: Olu ortu, toprak yogunlugu, toprak sikismasi, toprak nemi. Received (Gelis):  20.10.2016 -  Revised (Duzeltme):  28.11.2016 - Accepted (Kabul):  28.11.2016 Cite (Atif):  Duyar, A., Kinis, S., 2017.The effect of trekking activities on the some physical properties of soil in the fir forests in Bolu-Aladag.  Journal of the Faculty of Forestry Istanbul University  67(2): xxx-xxx. DOI: 10.17099/jffiu.xxxxx","PeriodicalId":17682,"journal":{"name":"Journal of the Faculty of Forestry Istanbul University","volume":" 8","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"The effect of trekking activities on the some physical properties of soil in the fir forests in Bolu-Aladag\",\"authors\":\"A. Duyar, S. 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Bu doga yuruyusunun olu ortu kalinligi, toprak yogunlugu, toprak nemi vb fiziksel ozelliklere etkisi incelenmistir. Calisma iki yil pes pese, iki ayri parselde ve ucer tekerrurlu olarak yapilmistir. Olu ortu kalinligi (cm), miktari (gr/m2) olarak belirlenmistir. Taze ve kurutulmus toprak yogunluklari (g/l) hacim silindirleri kullanilarak, toprak nemi (%) de taze ve kuru agirlik farkindan yararlanilarak belirlenmistir. Yapilan olcumler ve degerlendirmelerin sonucunda; doga yuruyusu yapilan alanda olu ortu kalinliginin azaldigi (r=0,568**), taze (r=0,440**) ve kurutulmus (r=0,423**) toprak yogunlugunda artisa neden oldugu belirlenmistir. Ancak toprak nemi uzerinde etkisi gorulmemistir. Kontrol alanina gore kiyaslandiginda cignenilen alan  topraginda ortalama %14 oraninda sikisma meydana geldigi bulunmustur. Doga yuruyusu esnasinda cignenen toprakta meydana fiziksel etkiler olu ortude ve toprakta sikismaya neden olmustur. 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引用次数: 0

摘要

摘要/ Abstract摘要:本文研究了徒步活动对森林地表的影响。在这项研究中,100人在测量区域排成一列。考察了徒步活动对土壤理化性质、土壤密度、土壤Toprak Nemi等的影响。该研究分两个独立的包裹进行,并在连续两年进行三次重复。取凋落物厚度cm和数量gr/m2。鲜土和干土容重(g/l)用体积圆柱体确定。土壤Toprak Nemi(%)由鲜重和干重计算差值确定。测量和评价的结果;结果表明,徒步旅行区奥鲁奥尔图喀里里吉斯减少(r = 0.568**),鲜土密度(r = 0.440**)和干土密度(r = 0.423**)增加。然而,未观察到Toprak Nemi对土壤的影响。根据对照区与践踏区相比,土壤中平均发生了14%的Sikisma。在徒步旅行过程中,土壤中物理效应的发生对凋落物和土壤产生压缩作用。因此,土壤入渗能力会降低,然后可能导致荒野和侵蚀。关键词:凋落物,土壤密度,土壤穿透力,Bolu-Aladag - goknar - ormanlarinda, Bolu-Aladag - goknar - ormanlarinda, Bolu-Aladag - goknar - ormanlarinda, Bolu-Aladag - goknar - ormanlarinda, Bolu-Aladag - goknar - ormanlarin, topragaga - etkisini。Calismada, 100, kisi, olc, alanindo, sila, halinur。但是,狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗狗卡利斯马伊基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基基。Olu ortu kalinligi (cm), miktari (gr/m2) olarak belirlenmistir。Taze ve kurutulmus toprak yogunluklari (g/l) haachim silindirleri kullanilarak, toprak nemi (%) de Taze ve kuru agirlik farkindan yararlanilarak belirlenmistir。亚皮兰水蛭的生长发育发育;Doga yuruyusu yapilan alanda olu ortu kalinliinin azaldigi (r= 0.568 **), taze (r= 0.440 **), kurutulmus (r= 0.423 **), toprak yogunlugunda artisen oldugu belirlenmistir。我想说的是,我的朋友们都很喜欢我的朋友们。[14]防治褐飞虱(褐飞虱)。Doga yuruyusu esnasinda cignenen toprakta meydana fiziksel -杀手(杀手)(杀手)(杀手)(杀手)(杀手)Dolayisiyla topragin与kappasitesini dusureck、devaminda yabanlask等具有较强的抗氧化能力。anhtar Kelimeler: Olu ortu, toprak yogunlugu, toprak sikismasi, toprak nemi。收稿(Gelis): 2016年10月20日-修订(Duzeltme): 2016年11月28日-接受(Kabul): 2016年11月28日引用(Atif): Duyar, A., Kinis, S., 2017。徒步活动对Bolu-Aladag冷杉林土壤某些物理性质的影响。伊斯坦布尔大学林业学院学报67(2):xxx-xxx。DOI: 10.17099 / jffiu.xxxxx
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The effect of trekking activities on the some physical properties of soil in the fir forests in Bolu-Aladag
The effect of trekking activities on the some physical properties of soil in the fir forests in Bolu-Aladag Abstract:  This study was conducted over the effect on forest floor of trekking activities. In this study, 100 people walked in single file on the measurement area. The impacts of this trekking activite were investigated on some physical properties such as Olu Ortu Kalinligi, soil density, soil Toprak Nemi, etc. The study was carried out in two seperate parcels and three replications in two consecutive years. Those were determinated as litter thikcness cm and amount gr/m2. Fresh and dried soil bulk densitys (g/l) were defined by using volume cylinders. Soil Toprak Nemi (%) was determined by using calculation differences of the fresh and dried weights. The results of the measurement and evaluation; determined that Olu Ortu Kalinligi was decreased (r = 0.568**), and densitys of fresh soil (r = 0.440**) and dried soil (r = 0.423**) were increased in the trekking area. However, the effect on the soil Toprak Nemi was not observed. Based on the con trol field compared to the trampled area the average a 14% a Sikisma has occurred in the soil. During the trekking, the occurring of physical effects in the soil caused to compress on the litter and soil. Therefore, the soil infiltration capacity will reduce, then it may lead to being wildness and erosion. Keywords:  Litter, soil density, soil penetration Bolu-Aladag goknar ormanlarinda doga yuruyusu faaliyetlerinin topragin bazi fiziksel ozelliklerine etkisi Ozet:  Bu calisma, Bolu Aladag goknar ormanlarinda, doga yuruyuslerinin topraga etkisini arastirmak icin yapilmistir. Calismada 100 kisi olcum alanindan tek sira halinde yurumustur. Bu doga yuruyusunun olu ortu kalinligi, toprak yogunlugu, toprak nemi vb fiziksel ozelliklere etkisi incelenmistir. Calisma iki yil pes pese, iki ayri parselde ve ucer tekerrurlu olarak yapilmistir. Olu ortu kalinligi (cm), miktari (gr/m2) olarak belirlenmistir. Taze ve kurutulmus toprak yogunluklari (g/l) hacim silindirleri kullanilarak, toprak nemi (%) de taze ve kuru agirlik farkindan yararlanilarak belirlenmistir. Yapilan olcumler ve degerlendirmelerin sonucunda; doga yuruyusu yapilan alanda olu ortu kalinliginin azaldigi (r=0,568**), taze (r=0,440**) ve kurutulmus (r=0,423**) toprak yogunlugunda artisa neden oldugu belirlenmistir. Ancak toprak nemi uzerinde etkisi gorulmemistir. Kontrol alanina gore kiyaslandiginda cignenilen alan  topraginda ortalama %14 oraninda sikisma meydana geldigi bulunmustur. Doga yuruyusu esnasinda cignenen toprakta meydana fiziksel etkiler olu ortude ve toprakta sikismaya neden olmustur. Dolayisiyla topragin gecirgenlik kapasitesini dusurecek, devaminda yabanlasmaya ve erozyona yol acabilecektir. Anahtar Kelimeler: Olu ortu, toprak yogunlugu, toprak sikismasi, toprak nemi. Received (Gelis):  20.10.2016 -  Revised (Duzeltme):  28.11.2016 - Accepted (Kabul):  28.11.2016 Cite (Atif):  Duyar, A., Kinis, S., 2017.The effect of trekking activities on the some physical properties of soil in the fir forests in Bolu-Aladag.  Journal of the Faculty of Forestry Istanbul University  67(2): xxx-xxx. DOI: 10.17099/jffiu.xxxxx
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