FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3096259329> ?p ?o ?g. }

• W3096259329 endingPage "119" @default.
• W3096259329 startingPage "97" @default.
• W3096259329 abstract "አህፅሮትኒቲሶልስ (Nitisols) በአብዛኛዉ ቀይ ወይም ቀይ-ቡናማ ቀለም  ያላቸዉ የአፈር ዓይነቶች ሲሆኑ በኢትዮጵያ ከፍተኛ አካባቢዎች በተለይም በደቡብ ምዕራብ ኢትዮጵያ ሰፊ የእርሻ መሬት ይሸፍናሉ፡፡ ይህ የአሰሳ ጥናት በ250 ሜትር ጥራት (ሪዞልዩሺን) የተወሰኑ የኒቲሶልስ ገፀ አምደ አፈሮችን በማዘጋጀት የሥነ ቅርፀ-አፈር (ሞርፎሎጂካል)፣ ፊዚካዊና ኬሚካዊ ባህሪያትን እንደዚሁም የንጥረነገር ይዘት ያጠቃልላል፡፡ ይህ በ46 የኒቲሶል ገፀ አምደ አፈሮች ላይ የተካሄደ ጥናት የአፈር ልኬተ አሲድጨው፣ የአፈር ዘአካል ካርቦን፣ ዓቢይና ንዑስ ንጥረምግቦች፣ የማዕድንና ጠቅላለ የንጥረነገሮችን ይዘት ምርመራና ትንተና የያዘ ነዉ፡፡ የዚህ ጥናት ዉጤት እንደሚያሳየዉ በኢትዮጵያ ከፍተኛ አካባቢ የሚገኘዉ የኒቲሶል መሰረታዊ የሥነ አፈር ባህርይ ይለያል፡፡ የዚህ አፈር ልኬተ አሲድጨው በ4.8 እና በ6.7 መካከል ሲሆን በጠንከራ እና አነስተኛ የአሲዳማነት ደረጃ ይመደባል፡፡ የዚህ አፈር የካርቦን፣ የናይተሮጅንና የድኝ (ሰልፈር) ይዘት በጣም ዝቅተኛ ሲሆን መጠናቸዉም በቅደም ተከተል 2.05፣ 0.18 እና 0.94 ሚ.ግ. በኪ.ግ. መሆኑን ያሳያል፡፡ ሆኖም በአፈር ዉስጥ የሚገኙ የፎስፎረስ (ከ2.40 እስከ 26.40 ሚ.ግ. በኪ.ግ) እና የፖታሲየም (ከ0.07 እስከ 2.77 ሴንቲሞል በከ.ግ) መጠን ሰፊ የሆነ ልዩነት የታየባቸዉ ሲሆን ይህም በአፈር-ሰር ቁሶችና በመሬት አጠቃቀም ልዩነት ምክንያት የተፈጠረ ሊሆን ይችላል፡፡ የንዑስ ንጥረምግቦችን በተመለከተ ደግሞ ይህ አፈር በብረት (Fe)፣ ማንጋኒዝ (Mn) እና ነሀስ (Zn) ንጥረ ነገሮች መጠን በጣም ከፍተኛ ሲሆን በመዳብ (Cu) እና በቦሮን (B) ይዘት ግን በጣም ዝቅተኛ ነዉ፡፡ በአንጻሩ ግን ይህ የአፈር ዓይነት በመጠነ አሉታ ሙል (CEC፣ አማካይ 41.93 ወይም ከ26 እስከ 57 ሴንቲሞል በኪ.ግ) እና በጨዋማ ንጥረነገር (base saturation፣ አማካይ 73% ወይም ከ50 እስከ 95%) መጠን በጣም ከፍተኛ ሲሆን በኤፒ አድማሰ አፈር (Ap horizon) ዉስጥ አማካይ የሲልት እና ሸክላ አፈር ስብርባሪ (ፍራክሽን) ንፃሬ (ሬሺዮ) 0.38 በመሆኑ ከፍተኛ ነዉ፡፡ ከሌሎች መሰል ኒቲሶል የአፈር ዓይነቶች አንጻር  በቀዳሚ ማዕድናት ይዘት በዋናነት ፊልድስፓር እና 2፡1 ፋይሎሲሊኬት (phyllosilicates) በዋናነት ማይካ በሸክላ አፈር ስብርባሪ ዉስጥ የሚገኙ ሲሆን ይህ አፈር በመካከለኛ ዕድሜ ክልል የሚገን ገና ያላረጀ መሆኑን ያሳያል፡፡ በዚህ አፈር ላይ ዘላቂ እርሻ ለማካሄድ በአፈር ዉስጥ ቅሬተ ዘአካል ማሳደግና እንደዚሁም የተመጣጠነ እና ትክክለኛ የአፈር ማዳበሪያ መጨመር ያስፈልጋል፡፡ በተጨማሪም በአለም አቀፍ የአፈር ሀብት (World Resource Base) ምደባ ዘዴ መሰረት የኒቶሶል ልዩ ገፀ አምደ አፈር ለንዑስ ኒቲሶል ልየታ የሚረዱ ተጨማሪ መመዘኛዎችን አካቷል፡፡  Abstract Nitisols cover an extensive area of the agricultural landscape in the Ethiopian highlands. This study outlines the morphological and physico-chemical properties, and the mineralogical and total elemental composition of some Nitisol profiles based on soil survey at 250 m resolution. Analytical data of 46 Nitisol profiles were studied for soil pH, organic carbon (OC) and some macro and micronutrients, and mineralogical and total elemental composition. Results showed that Nitisols of the Ethiopian highlands differ in some fundamental ways from the pedogenetic characteristics often referred to in the mainstream soil science literature. The soils in this study are strongly to moderately acidic with pH of 4.8-6.7, and very low in OC, TN and sulfur (S) with mean values of 2.05%, 0.18% and 0.94 mg/kg. But levels of available phosphorus (AP) and exchangeable K showed wide variation (2.40 to 26.40 mg/kg P and 0.07 to 2.77 cmol (+)/kg K), reflecting differences in parent materials and land use. Considering micronutrients, the soils are very high in iron (Fe), manganese (Mn) and zinc (Zn) but severely deficient in copper (Cu) and boron (B). Conversely, the soils are very high in CEC (mean 41.93, range 26-57 cmol (+)/kg) and base saturation (mean 73%, range of 50-95%), and mean silt/clay ratio of 0.38 in the Ap horizon is rated high. Mineralogical composition of primary minerals (chiefly feldspars) and 2:1 phyllosilicates (mainly mica) in the clay fraction, suggests that the soils are still young and cannot be qualified as “highly weathered soils” in contrast with other tropical Nitisols. At a local level, the results suggest that sustainable agricultural production on these soils depends on the replenishment of organic matter and application of fertilizers in proper balance and right amounts. Also, the distinct characteristics of Nitisol profiles described provide additional diagnostic criteria to distinguish subunits of Nitisols (i.e., third level) under the WRB system of classification." @default.
• W3096259329 created "2020-11-09" @default.
• W3096259329 creator A5062654295 @default.
• W3096259329 creator A5077769862 @default.
• W3096259329 date "2020-10-31" @default.
• W3096259329 modified "2023-09-27" @default.
• W3096259329 title "Mineralogical and Physicochemical Properties of Nitisols In The Ethiopian Highlands" @default.
• W3096259329 cites W1489987127 @default.
• W3096259329 cites W173291398 @default.
• W3096259329 cites W1907010074 @default.
• W3096259329 cites W1979445010 @default.
• W3096259329 cites W1984893196 @default.
• W3096259329 cites W2013334942 @default.
• W3096259329 cites W2053150014 @default.
• W3096259329 cites W2100063715 @default.
• W3096259329 cites W2112979714 @default.
• W3096259329 cites W2159620994 @default.
• W3096259329 cites W2162457850 @default.
• W3096259329 cites W2183659348 @default.
• W3096259329 cites W2314942182 @default.
• W3096259329 cites W2331197984 @default.
• W3096259329 cites W2745577199 @default.
• W3096259329 cites W2907328678 @default.
• W3096259329 cites W2909511481 @default.
• W3096259329 cites W81725153 @default.
• W3096259329 hasPublicationYear "2020" @default.
• W3096259329 type Work @default.
• W3096259329 sameAs 3096259329 @default.
• W3096259329 citedByCount "0" @default.
• W3096259329 crossrefType "journal-article" @default.
• W3096259329 hasAuthorship W3096259329A5062654295 @default.
• W3096259329 hasAuthorship W3096259329A5077769862 @default.
• W3096259329 hasConcept C107872376 @default.
• W3096259329 hasConcept C149849071 @default.
• W3096259329 hasConcept C158787203 @default.
• W3096259329 hasConcept C159390177 @default.
• W3096259329 hasConcept C159750122 @default.
• W3096259329 hasConcept C178790620 @default.
• W3096259329 hasConcept C185592680 @default.
• W3096259329 hasConcept C197484155 @default.
• W3096259329 hasConcept C198072978 @default.
• W3096259329 hasConcept C199289684 @default.
• W3096259329 hasConcept C39432304 @default.
• W3096259329 hasConcept C50516716 @default.
• W3096259329 hasConcept C528890316 @default.
• W3096259329 hasConceptScore W3096259329C107872376 @default.
• W3096259329 hasConceptScore W3096259329C149849071 @default.
• W3096259329 hasConceptScore W3096259329C158787203 @default.
• W3096259329 hasConceptScore W3096259329C159390177 @default.
• W3096259329 hasConceptScore W3096259329C159750122 @default.
• W3096259329 hasConceptScore W3096259329C178790620 @default.
• W3096259329 hasConceptScore W3096259329C185592680 @default.
• W3096259329 hasConceptScore W3096259329C197484155 @default.
• W3096259329 hasConceptScore W3096259329C198072978 @default.
• W3096259329 hasConceptScore W3096259329C199289684 @default.
• W3096259329 hasConceptScore W3096259329C39432304 @default.
• W3096259329 hasConceptScore W3096259329C50516716 @default.
• W3096259329 hasConceptScore W3096259329C528890316 @default.
• W3096259329 hasIssue "4" @default.
• W3096259329 hasLocation W30962593291 @default.
• W3096259329 hasOpenAccess W3096259329 @default.
• W3096259329 hasPrimaryLocation W30962593291 @default.
• W3096259329 hasRelatedWork W1134792490 @default.
• W3096259329 hasRelatedWork W1601648168 @default.
• W3096259329 hasRelatedWork W200490445 @default.
• W3096259329 hasRelatedWork W2007024831 @default.
• W3096259329 hasRelatedWork W2018624451 @default.
• W3096259329 hasRelatedWork W2083749691 @default.
• W3096259329 hasRelatedWork W2087005876 @default.
• W3096259329 hasRelatedWork W2099580332 @default.
• W3096259329 hasRelatedWork W2109571062 @default.
• W3096259329 hasRelatedWork W2114442533 @default.
• W3096259329 hasRelatedWork W2184818676 @default.
• W3096259329 hasRelatedWork W2230326233 @default.
• W3096259329 hasRelatedWork W2400397367 @default.
• W3096259329 hasRelatedWork W2553330238 @default.
• W3096259329 hasRelatedWork W2763251599 @default.
• W3096259329 hasRelatedWork W3004717588 @default.
• W3096259329 hasRelatedWork W3044091322 @default.
• W3096259329 hasRelatedWork W3089624330 @default.
• W3096259329 hasRelatedWork W3094223563 @default.
• W3096259329 hasRelatedWork W2178579753 @default.
• W3096259329 hasVolume "30" @default.
• W3096259329 isParatext "false" @default.
• W3096259329 isRetracted "false" @default.
• W3096259329 magId "3096259329" @default.
• W3096259329 workType "article" @default.