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Water-air properties of Grodan® Master rockwool

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(1)Acta Agrophysica, 2007, 10(1), 113-120. :à$. &,:2&,:2'12-PO:,(75=1(:(à1<0,1(5ALNEJ. GRODAN® MASTER. Monika Jaroszuk-6LHURFLVND URGRZLVND$NDGHPLD5ROQLF]D VNLHJR-069 Lublin. ,QVW\WXW*OHER]QDZVWZDL.V]WDáWRZDQLD XO6/HV]F]\. e-mail: monika.jaroszuk@ar.lublin.pl. S t r e s z c z e n i e . PrzeproZDG]RQR EDGDQLD ZáDFLZRFL ZRGQR-SRZLHWU]Q\FK ZHáQ\ PLQHUDOQHM GRODAN® 0DVWHU : SUDF\RPyZLRQRV]F]HJyáRZRWHZáDFLZRFLNWyUHQDOH*\X]QDü]DEDUG]R ZD*QH SU]\ RFHQLH VWDQX IL]\F]QHJR SRGáR*\ Z SRMHPQLNDFK 6 WR SHáQD SRMHPQRü ZRGQD SRMHPQikowa poMHPQRü ZRGQD F]\OL  ]DZDUWRü  ZRG\  RGSRZLDGDMFD  SRWHQFMDáRZL – N3D ]DZDUWRü SRZLHWU]D Z VWDQLH SRMHPQLNRZHM SRMHPQRFL ZRGQHM – N3D

(2)  D WDN*H UHWHQFMD ZRG\ QDMáDWZLHM GoVW SQHM RG –0,98 do – N3D %DGDQD ZHáQD FKDUDNWHU\]RZDáD VL  EDUG]R GREU\PL ZáDFLZRFLDPL z SXQNWX ZLG]HQLD SRWU]HE SURGXNFMLRJURGQLF]HMZSRMHPQLNDFKEDUG]RGX*SHáQSRMHPQRFLZRGQ – 12,40 kgÂNJ-1DSU]HGHZV]\VWNLPZ\MWNRZRZ\VRNSRMHPQLNRZSRMHPQRFLZRGQ– 11,23 kgÂNJ1 . 3RG Z]JO GHP ZáDFLZRFLSRZLHWU]Q\FKZHáQ PLQHUDOQUyZQLH*QDOH*\RFHQLüSR]\W\ZQLH Pojem3 -3 QRü SRZLHWU]QD Z VWDQLH SRMHPQLNRZHM SRMHPQRFL ZRGQHM – N3D

(3)  Z\QRVLáD  P ÂP , 3 -3 a ZL F E\áD QLH]QDF]QLH QL*V]D RG ZDUWRFL NU\W\F]QHM F]\OL  P ÂP  -X* MHGQDN VSDGHN SRWHn3 -3 FMDáX GR – N3D VSRZRGRZDá Z]URVW SRMHPQRFL Sowietrznej do 0,46 m ÂP  SU]\ EDUG]R GX*HM . ]DZDUWR FL ZRG\  NJÂNJ. -1. . *. *.

(4)  .V]WDáWXM F RGSRZLHGQLR SRWHQFMDá ZRG\ PR QD Z SRGáR X ] ZHá. -powietrznych. 6 á R Z D  N O X F ] R w e : ZHáQDPLQHUDOQDZáDFLZRFLZRGQR-powietrzne. Q\PLQHUDOQHMGREUDüLGHDOQ\XNáDGVWRVXQNyZZRGQR. 3. :67. W krajach Unii Europejskiej, a od lat 90-W\FK;;ZLHNXWDN*HZ3ROVFHQDj*. EDUG]LHM UR]SRZV]HFKQLRQ\P SRGáR HP RJURGQLF]\P MHVW ZHáQD PLQHUDOQD. *. . 5XPSHO 

(5)  : XSUDZDFK EH]JOHERZ\FK SRGáR D]ZHáQ\PLQHUDOQHM]DMPXM . obecnie. . *. *. o-. SLHUZV]HPLHMVFHZ\SU]HG]DM FQDMZD QLHMV]HGRQLHGDZQDSRGáR DZ\SU. FLHM ]ZUDFD VL  XZDJ  QD SRGVWDZRZ ZDG  ZHáQ\ F]\OL WUXGQRFL Z VNáDGRZDQLX L XW\OL]DFML RGSDGyZ RUD] V]XND PR*OiZRFL ]DVWSLHQLD PDWHULDáDPL áDWZLHMV]\PL GR ]DJRVSRGDURZDQLD (Komosa 2002,. GXNRZDQH QD ED]LH WRUIX -HGQDN FRUD] F].

(6) M. JAROSZUK-6,(52&,6.$. 114. . %DELN  .OHLEHU L .OHLEHU 

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(14) :à$. &,:2&,:2'12-PO:,(75=1(:(à1<0,1(5ALNEJ. . 115. *. W\ZQ\ L ZHJHWDW\ZQ\ UR OLQ Z FHOX SURZDG]HQLD SURGXNFML QD QDMZ\ V]\P S. *. o-.  zapewnia najlepszy transSRUWZRG\ZFDá\PSU]HNURMXPDW\3U]\F]\QLDVL WRGR UR]ZRMX V\VWHPX NRU]HQLRZHJR D Z UH]XOWDFLH GR RVLJQL FLD Z\VRNLHJR SOonu GRVNRQDáHMMDNRFL ZZZJURGDQSO

(15)  3UyENL ZHáQ\ PLQHUDOQHM GR R]QDF]HQLD ZáDFLZRFL ZRGQR-powietrznych SREUDQRZV]HFLXSRZWyU]HQLDFKEH]SRUHGQLR]PDW\RJUXERFL cm do meta3 ORZ\FK F\OLQGUyZ R REM WRFL  FP  RGFLQDMF QDGPLDU PDW\ SR  cm) z gór-. ]LRPLHSU]H]FDá\VH]RQ:HáQDWDPDGZLHZDUVWZ\ZáyNLHQRUy QHMJ VWR FLFR. QHM L GROQHM VWURQ\ F\OLQGUD 3UyENL GRSURZDG]RQR GR VWDQX SHáQHJR  QDV\FHQLD. . . ZRG N3D1DVW SQLHZ\NRQDQRR]QDF]HQLD]DZDUWR FLZRG\RSRWHQFMDáDFK. –0,24 kPa; –0,98 kPa; –3,10 kPa; –9,81 kPa; –15,54 kPa; –30,99 kPa i –49,03 kPa . . Z NRPRUDFK QLVNRFL QLHQLRZ\FK QD SRURZDW\FK Sá\WDFK FHUDPLF]Q\FK PHWRG . Richardsa. . – N3DZZHáQLHRGSRZLDGDSRMHmnikowej poMHPQRFLZRGQHMGODSRMHPQLNDRZ\VRNRFL FP]D –9,81 kPa – polowej pojemQRFLZRGQHMJOHEQDWXUDOQ\FKRSR]LRPLHZRG\JUXQWRZHMQDJá EoNRFLP 2]QDF]HQLH ]DZDUWRFL ZRG\ R SRWHQFMDáDFK –155,4 kPa (punkt silnego zahaPRZDQLD Z]URVWX URlin); – N3D SXQNW FDáNRZLWHJR ]DKDPRZDQLD Z]URVWX UoOLQ

(16)  L – N3D SXQNW WUZDáHJR ZL GQL FLD

(17)  Z\NRQDQR Z NRPRUDFK Z\VRNRFiQLHQLRZ\FK VWRVXMF MDNR PHPEUDQ  FHORIDQ =DZDUWRü ZRG\ RGSRZLDGDMF SoWHQFMDáRZL – N3D PDNV\PDOQ KLJURVNRSLMQRü

(18)  R]QDF]RQR Z VXV]DUFH SUy* niowej nad 10% H2SO4. = X]\VNDQ\FK Z\QLNyZ VSRU]G]RQR FKDUDNWHU\VW\N  SRWHQFMDá ZRG\ – wilgot-1 QRü Z\UD*DMF ]DZDUWRü ZRG\ Z NJÂNJ . Obliczono poszczególne kategorie retenFMRQRZDQHM ZRG\ WM ZRG  JUDZLWDF\MQ RG  GR –0,98 N3D

(19)  ZRG  QDMáDWZLHM GoVW SQGODUROLQ RG–0,98 do –N3D

(20) ZRG X*\WHF]Q GRVW SQGODUROLQ

(21)  RG– 9,81 do – N3D

(22)  ZRG  QLHGRVW SQ GOD UROLQ SRQL*HM –1554 kPa). Wszystkie 3 –3 X]\VNDQHZ\QLNLZ\UD*RQRUyZQLH*ZP ÂP . 'ODND*GHMZDUWRFLSRWHQFMDáXREOLF]RQRUyZQLH*SRMHPQRüSRZLHWU]Q na podVWDZLH SHáQHM SRMHPQRFL ZRGQHM L SRMHPQRFL ZRGQHM REM WRFLRZHM Z RGSo3 -3 ZLHGQLPVWDQLHZ\V\FHQLDSRGáR*DZRG:\QLNLSRGDQRZP ÂP . =DZDUWR ü ZRG\ R SRWHQFMDOH. . . . * VWR ü ZHáQ\ Z\]QDF]RQR PHWRG  JUDZLPHWU\F]Q  QD SRGVWDZLH VWRVXQNX. ºC do wyjFLRZHM REM WRFL. PDV\ PDWHULDáX Z\VXV]RQHJR Z WHPSHUDWXU]H . *. 3. –3. *. SRGáR D FP

(23) :\QLNLZ\UD RQRZ0JÂP. .. WYNIKI I DYSKUSJA. . . %DGDQDZHáQDFKDUDNWHU\]RZDáDVL EDUG]RGREU\PLZáD FLZR FLDPL]SXQNWX. widzenia potrzeb produkcji ogrodniczej w pojemniNDFK EDUG]R GX* SHáQ So-1 MHPQRFLZRGQ – 12,40 kgÂNJ DSU]HGHZV]\VWNLPZ\MWNRZRZ\VRN pojem-.

(24) M. JAROSZUK-6,(52&,6.$. 116. -1. .    – 11,23 kgÂNJ  WDE 

(25)  &HFK\ WH Z\UD*RQH Z VWo3 -3 VXQNXGRREM WRFLSRGáR*DSU]\MPRZDá\ZDUWRFLL m ÂP . Przekrocze3 -3 nie wartoFLP ÂP ZVWDQLHSHáQHMSRMHPQRFLZRGQHMZ\QLNDáR]QDS F]QLHQLD materiaáX 3RMHPQRü ZRGQD ZHáQ\ PLQHUDOQHM SU]\ SRWHQFMDOH ZRG\ –9,81 kPa FRRGSRZLDGDZJOHELHQDWXUDOQHMVWDQRZLSRORZHMSRMHPQRFLZRGQHM

(26) Z\QosiáD W\ONR  NJÂNJ-1 (0,02 m3ÂP-3

(27) 1DVWSLáZL FZW\P]DNUHVLHSRWHQFMDáXZ\MtNRZRGX*\VSDGHN]DZDUWRFLZRG\ZSRUyZQDQLXGRVWDQXSRMHPQLNRZHMSRMHPQoFLZRGQHM U\V

(28) . QLNRZ  SRMHPQR FL  ZRGQ . 14 12. θ (kgÂkg-1). 10 8 6 4 2 0 0,01. 0,1. 1. 10. 100. 1000. 10000. |Ψ|| (kPa) Rys. 1. &KDUDNWHU\VW\NDSRWHQFMDáZRG\

(29)

(30) – ZLOJRWQRü 

(31) ZHáQ\PLQHUDOQHM Grodan Fig. 1. Water potential (

(32) ) – moisture ()” characteristic of Grodan rockwool. . . : XSUDZLH UR OLQ Z SRMHPQLNDFK SU]\ SRWHQFMDOH ZRG\ RGSRZLDGDM F\P. –9,81 kPa MX* MHVW ]DOHFDQH QDZDGQLDQLH SRGF]DV JG\ Z JOHELH MHVW WR VWDQ QDMNorzystniejszego nasycenia woG $E\ SUDZLGáRZR RFHQLü ZáDFLZRFL ZRGQH ZHáQ\ PLQHUDOQHMQLHRG]RZQHMHVWZL FRNUHOHQLHZDUWRFLUHWHQFMLSRGVWDZRZ\FKNDWHJo. ULLZRG\5HWHQFMDGHF\GXM FDRSURGXNFMLZSRMHPQLNDFKWRUHWHQFMDZRG\QDMáDWZLHM. . .  d–0,98 do – N3D

(33)  : SRGáR*X ] ZHáQ\ warWRü WHM UHWHQFML E\áD Z\MWNRZR GX*D L Z\QRVLáD  NJÂNJ-1 (0,91 m3ÂP-3). GRVW SQHMGODUR OLQ]DZLHUDM FDVL ZSU]HG]LDOHRGSRMHPQLNRZHMSRMHPQR FLZR. . QHM GR SRORZHM SRMHPQR FL ZRGQHM RG. *. *. WDE

(34)  5HWHQFMD ZRG\ X \WHF]QHM QDMZD QLHMV]D Z SURGXNFML SRORZHM Z ZHáQLH. *. PLQHUDOQHM E\áD G]LHVL FLRNURWQLH QL V]D. – 0,17 kgÂNJ-1 (0,01 m3ÂP-3

(35)  -HGQDN*H WR.

(36) :à$. &,:2&,:2'12-PO:,(75=1(:(à1<0,1(5ALNEJ. . . . 117. . i-. QLH RQD GHF\GXMH R LOR FL ZRG\ NWyU  Z\NRU]\VWXM  UR OLQ\ Z XSUDZLH SRMHPQ. kowej. W tym systePLH XSUDZ\ SRGáR*H XWU]\PXMH ZEUHZ VLOH JUDZLWDFML ZRG  o potencjale odpoZLDGDMF\PSRMHPQLNRZHMSRMHPQRFLZRGQHMNWyUD]DOH*\RG ZLHONRFL L NV]WDáWX GRQLF]NL NRVWNL OXE PDW\ D GOD VWDQGDUGRZego pojemnika o Z\VRNRFLFPUyZQDMHVW–0,98 kPa (Argo 1998, Fonteno 1988). Tabela 1.:\EUDQHSRMHPQRFLZRGQHZHáQ\PLQHUDOQHM*URGDQ Table 1. Selected water capacities of Grodan rockwool . . 3HáQDSRMHPQR üZRGQD. 3RMHPQLNRZDSRMHPQR üZRGQD. (0,0 kPa) Full water capacity. (–0,98 kPa) Container water capacity. PoloZDSRMHPQRüZRGQD (–9,81 kPa) Field water capacity. (kgÂNJ-1). (m3ÂP-3). (kgÂNJ-1). (m3ÂP-3). (kgÂNJ-1). (m3ÂP-3). 12,40. 1,02. 11,23. 0,92. 0,18. 0,02. Tabela 2.5HWHQFMDUy*Q\FKNDWHJRULLZRG\ZHáQ\PLQHUDOQHM*URGDQ Table 2. Grodan rockwool retention of different water categories. *. 5HWHQFMDZRG\QDMáDWZLHMGRVW SQHM. 5HWHQFMDZRG\X \WHF]QHM. (od –0,98 do –9,81 kPa) Easily available water retention (from –0.98 to –9.81 kPa). (od –9,81 do –1554 kPa) Useful water retention (from –9.81 to –1554 kPa). Retencja wody QLHGRVW SQHM SRQL*HM–1554 kPa) Unavailable water retention (below –1554 kPa). (kgÂNJ-1). (m3ÂP-3). (kgÂNJ-1). (m3ÂP-3). (kgÂNJ-1). (m3ÂP-3). 11,05. 0,91. 0,17. 0,01. 0,01. 0,001. Tabela 3.* VWRüLZ\EUDQHSRMHPQRFLSRZLHWU]QHZHáQ\PLQHUDOQHM*URGDQ Table 3. Bulk density and selected air capacities of Grodan rockwool . . 3RMHPQLNRZDSRMHPQR üSRZLHWU]QD. 3RORZDSRMHPQR üSRZLHWU]QD. Bulk density (MgÂP-3). (–0,98 kPa) Container air capacity (m3ÂP-3). (–9,81 kPa) Field air capacity (m3ÂP-3). 0,08. 0,09. 1,00. . * VWR ü. NalH*\ WX SRGNUHOLü ]GHF\GRZDQH Uy*QLFH Z RFHQLH Uy*Q\FK NDWHJRULL ZRG\ * oGXNFMLNDWHJRULDZRG\F]\OLZRGDX*\WHF]QD RG–9,81 do –1554 kPa), w uprawie w pojemnikach stanowi jedynie rezHUZ 3RGVWDZJRVSRGDUNLZRGQHMZXSUDZLH SRMHPQLNRZHM MHVW QDMVáDELHM XWU]\P\ZDQD SU]H] ID]  VWDá ZRGD ]DMPXMFD QDjZ QDWXUDOQHM JOHELH L SRGáR DFK Z SRMHPQLNDFK 1DMFHQQLHMV]D Z SRORZHM SU. . ZL NV]H SRU\ NWyUD Z JOHELH V]\ENR RGSá\ZD Z Já E SHGRQX SRG ZSá\ZHP VLá\.

(37) M. JAROSZUK-6,(52&,6.$. 118. *. *. .  i-. JUDZLWDFML : SRMHPQLNX W  ZRG  PR QD ]DWU]\PDü Z SRGáR X L XGRVW SQLü M  UR O. * LORü ZRG\ QDMáDWZLHM GRVW SQHM GOD. QRP :HáQD PLQHUDOQD ]DSHZQLD EDUG]R GX. . UR OLQ FR MHVW QLH]Z\NOH FHQQH Z ZDUXQNDFK XSUDZ\ Z SRMHPQLNDFK UH]HUZD. w postaci retencji ZRG\X*\WHF]QHMMHVWWXQLHZLHONDFRRF]\ZLFLHQLHMHVWZDG bioUF SRG XZDJ  PR*OLZRFL VWDáHJR X]XSHáQLDQLD SREUDQHM SU]H] UROLQ\ ZoG\ 3RG Z]JO GHP ZáDFLZRFL SRZLHWU]Q\FK ZHáQ  PLQHUDOQ UywQLH* QDOH*\ RFHQLü SR]yW\ZQLH 3RMHPQRü SRZLHWU]QD Z VWDQLH SRMHPQLNRZHM SRMHPQRFL wodnej (– N3D

(38)  Z\QRVLáD  P3ÂP-3 D ZL F E\áD QLH]QDF]QLH QL*V]D RG 3 -3 ZDUWRFL NU\W\F]QHM F]\OL  P ÂP (tab.3). Natomiast w stanie polowej po3 -3 MHPQRFL ZRGQHM SRMHmQRü SRZLHWU]QD Z\QRVLáD D*  P ÂP  FR ZLDGF]\ o W\P *H Z MHV]F]H QDS F]QLDá\P PDWHULDOH ZRGD ]DMPXMH PLQLPDOQ REM WRü a QLHPDO ZV]\VWNLH SRU\ Z\SHáQLRQH V SRZLHWU]HP .V]WDáWXMF RGSRZLHGQLR SRWHnFMDá ZRG\ PR*QD ZL F Z SRGáR*X ] ZHáQ\ PLQHUDOQHM GREUDü LGHDOQ\ XNáDG VWRVXnków wodno-powietrznych. 1DOH*\]ZUyFLüXZDJ  *HZ *DGQ\PZ\SDGNXQLHPR*QDRFHQLDüVWRVXQNyw wodno-SRZLHWU]Q\FK ZHáQ\ PLQHUDOQHM MHG\QLH QD SRGVWDZLH SRPLDUyZ SRORZHM . . SRMHPQR FLZRGQHMLSRZLHWU]QHM3URZDG]LáRE\WRGRVWZLHUG]H R]GHF\GRZDQHM. s *  5HDVXPXMFZ\QLNLEDGDSU]HGVWDZLRQ\FKZQLQLHMV]HMSUDF\PR*QD]GHFy® GRZDQLH SRWZLHUG]Lü SU]\GDWQRü ZHáQ\ PLQHUDOQHM *52'$1 Master do proGXNFMLRJURGQLF]HMZSRMHPQLNDFK]FDáSHZQRFLPR*QDMSROHFLüGRXSUDZ\ nawet QDMEDUG]LHM Z\PDJDMF\FK UROLQ :HáQD PLQHUDOQD PR*H ] SRZRG]HQLHP ]DVW SRZDü Z SURGXNFML RJURGQLF]HM WRUI Z\VRNL FR QLHZWSOLZLH SU]\F]\QL VL  GR RFKURQ\ WRUIRZLVN ]DJUR*RQ\FK QDGPLHUQ HNVSORDWDFM QD FR V]F]HJyOQ XZDJ ]ZUDFDZVZRLFKG\UHNW\ZDFKViedliskowych Unia Europejska. Dla stwoSU]HZDG]HSRZLHWU]DZW\PPDWHULDOHLQLHGRERU]HZRG\FRPRJáRE\ZU F]G\. NZDOLILNRZDüZHáQ PLQHUDOQ MDNRSRGáR HZXSUDZLHUR OLQ. -powietrznych konieczne jest oczynFMDáZRG\-ZLOJRWQRüZSU]HG]LDOHSRWHQFMDáXZRG\RGGR–9,81 kPa. U]HQLD RSW\PDOQHJR XNáDGX VWRVXQNyZ ZRGQR. . ZL FLH XPLHM WQH VWHURZDQLH QDZDGQLDQLHP QD SRGVWDZLH FKDUDNWHU\VW\NL SRWH. WNIOSKI. 1.. = SXQNWX ZLG]HQLD SRWU]HE SURGXNFML RJURGQLF]HM Z SRMHPQLNDFK ZHáQD.  oFLDPLZRGQR– powietrznymi. W stanie pojemnikowej poMHPQRFL ZRGQHM – N3D

(39)   SRGáR*H –1 WRXWU]\PXMHEDUG]RGX*LORü wody (11,23 kgÂNJ

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(42) :à$. &,:2&,:2'12-PO:,(75=1(:(à1<0,1(5ALNEJ. 119. *H D*  SHáQHM SRMHPQRFL ZRGQHM ZHáQ\VWDQRZLZRGDQDMáDWZLHMGRVW SQDGODUROLQ RG –0,98 do –9,81 kPa), czyli. 2.. . 1D SRGNUH OHQLH ]DVáXJXMH IDNW. najcenniejsza kategoria wody w uprawie pojemnikowej. 3. 3RGVWDZ RFHQ\ ZáDFLZRFL ZRGQR-SRZLHWU]Q\FK ZHáQ\ PLQHUDOQHM SRZLQQD E\ü SHáQD FKDUDNWHU\VW\ND SRWHQFMDá ZRG\-ZLOJRWQRü ]H V]F]ególnym XZ]JO GQLHQLHPVWDQXSRMHPQLNRZHMSRMHPQRFLZRGQHMF]\Oi –0,98 kPa. 4. :ZHáQLHPLQHUDOQHMZSU]HG]LDOHSRWHQFMDáXRG–0,98 kPa do –9,81 kPa QDVW SXMH JZDáWRZQD ]PLDQD ZDUXQNyZ ZRGQR-SRZLHWU]Q\FK SROHJDMFD QD QLePDOFDáNRZLW\PRGZRGQLHQLXSRGáR*DZVWDQLHSRWHnFMDáXZRG\–9,81 kPa.. 0,(11,&7:2. 3,. Argo W., 1998. Root medium physical properties. Hort. Technology., Aleksandria, 481-485. Babik J., 2006. 3RGáR*DRJURGQLF]HGRXSUDZ\RJyUNDV]NODUQLRZHJRDOWHUQDW\ZQHGODZHáQ\PLQeralnej. Acta Agrophysica, 7(4), 809-820. Fonteno W. C., 1988. Know your media, the air, water and plant responses to rockwool-amended media. J. Amer. Soc. Hort. Sci., 115(3), 375-381. Fonteno W. C., 1989. An approach to modeling air and water status of horticultural substrates. Acta Hort., 238, 67-74. Fonteno W.C., 1993. Problems & considerations in determining physical properties of horticultural substrates. Acta Hort., 342, 197-204. -DURV]XN 0 6áRZLVND--XUNLHZLF] $  &KDUDNWHU\VW\ND SRGVWDZRZ\FK ZáDFLZRFL ZRGQRSRZLHWU]Q\FK SRGáR*\ RJURGQLF]\FK VWRVRZDQ\FK Z XSUDZLH SRMHPQLNRZHM Zesz. Probl. Post. Nauk Roln., 504, 105-110. .OHLEHU7.OHLEHU$8SUDZDRJyUNDZSRGáR*DFKLQHUWQ\FKLRUJDQLF]Q\FK+DVáRRJURGQicze, 2. .RPRVD $  3RGáR*D LQHUWQH – SRVW S F]\ LQHUFMD" 0DW .RQI Ä$NWXDOQH WUHQG\ Z SURGXNFML L stosowaniu SRGáR*\RJURGQLF]\FK´/XEOLQ-7 czerwca, 15-31. 1RZDN-6:áDFLZRFLSRZLHWU]QR-ZRGQHSRGáR*\RJURGQLF]\FK3UREO3RVW Nauk Roln., 504, 175-184. . *. 2 ZLHFLPVNL :  $NWXDOQH WHQGHQFMH Z Z\NRU]\VWDQLX SRGáR \ QLHRUJDQLF]Q\FK Z XSUDZDFK SRG. Nauk Roln., 429, 9-13. Rumpel J., 1998. Tradycyjne i nowe substraty uprawowe oraz problematyka ich stosowania. Zesz. Probl. Post. Nauk Roln., 461, 47-66. 6áDZLVNL&6REF]XN+$:DOF]DN57 Hydrofizyczne charakter\VW\NLSRGáR*\RJURdniczych DGRVW SQRüZRG\GODUROLQ=HV]3UREO3RVW1DXN5ROQ-278. www.grodan.pl RVáRQDPL=HV]3UREO3RVW.

(43) 120. M. JAROSZUK-6,(52&,6.$. WATER-AIR PROPERTIES OF GRODAN® MASTER ROCKWOOL Monika Jaroszuk-6LHURFLVND Institute of Soil Science and Environment Management, Agricultural University XO6/HV]F]\VNLHJR-069 Lublin e-mail: monika.jaroszuk@ar.lublin.pl A b s t r a c t . A study was carried out on the water-and-air properties of rockwool GRODAN® Master. The paper presents a detailed discussion of those properties which have should be considered as very important for the estimation of the physical condition of the beds in containers. These are: full water-capacity, container water capacity, i.e. the contents of water corresponding to the potential of –0.98 kPa, air content in the state of the container water capacity (–0.98 kPa), as well as the retention of easily available water, from –0.98 to –9.81 kPa. The rockwool under study was characterized by very good properties from the point of view of the need of garden production in containers: quite a considerable full water capacity – 12.40 kg kg-1, and, above all, an exceptionally high container water capacity – 11.23 kg kg-1. As for the air properties, the mineral wool should be also estimated in a positive way. Its air capacity in the state of box water capacity (–0.98 kPa) was 0.09 m3 m-3, and so it was insignificantly lower than the critical value of 0.10 m3 m-3. It is possible to establish an ideal system of water and air relationship by suitable forming of the water potential in the bed of the rockwool. K e y w o r d s : rockwool, water and air properties.

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