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https://mi21.vsb.cz/sites/mi21.vsb.cz/files/unit/matem_modelovani_elektromag_poli_3.pdf
v Časové změny magnetického pole indukuj́ı elektrické pole, které p̊usob́ı proti těmto změnám: ∮ ∂Σ(t) E(x, t)dl(x) = − ∂ ∂t ∫ Σ(t) B(x, t) · n(x) dS(x).
https://advances.vsb.cz/data/articles/2025/Vol%2023,%20No%201/Joint%20Power%20Control%20and%20Relay%20Selection%20with%20Short%20Packet%20Communications%20under%20Co-channel%20Interference.pdf
source (S), L relay nodes (R1, ..., RL) ∗, and one destination (U). It is assumed that L relays belong to one cluster [23]. All relays are affected by the
https://homel.vsb.cz/~s1a64/la_it.html
materi�ly. Z. Dost�l, V. Vondr�k: Line�rn� algebra L. �indel, O. Vlach: Analytick� geometrie P.�armanov�: Sb�rka ne�e�en�ch p��klad� z line�rn� algebry L. �indel: Sb�rka �e�en
https://transactions.fs.vsb.cz/2016-2/2020.pdf
Analysis, vol. 2013, Article ID 972371, 14 pages, 2013. doi:10.1155/2013/972371 [6] LIPING, Z., CHENG-CHEW, L., YIPING, C., AND HAMID, R. K., “Tracking Mobile
https://advances.vsb.cz/data/articles/2012/Vol%2010,%20No%204/Computer%20Science%20and%20Information%20Technology/An%20Approach%20to%20Personalized%20Search%20within%20Distributed%20Repository%20of%20Visual%20Data.pdf
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Thesis. The Technical University of Kosice. [4] DJENOURI, D., L. KHELLADI and N. BADACHE. A Survey of Security Issues in Mobile
https://mi21.vsb.cz/sites/mi21.vsb.cz/files/unit/laplace2_krok.pdf
0+) = x ′0, . . . , x (n−1)(0+) = x (n−1) 0 . (3) Aplikace Laplaceovy transformace Označme L(x(t)) = X (p) a
https://transactions.fs.vsb.cz/2012-1/1908.pdf
L of the beam is equidistantly divided into n parts with the step n LΔ , where node "0" is at the distance x = 0 m and node "
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http://geologie.vsb.cz/Sedimentologie/textova%20cast/klasifikace%20sedimentarnch%20hornn.htm
ji se cituje Smith (1978): �Sediment je produkt akumulace materi�lu poch�zej�c�ho ze zv�tral�ch a erodovan�ch hornin a donesen�ho na m�sto ulo�en� bu�to jako pevn� ��stice nebo v roztoku. Materi�
http://geologie.vsb.cz/PETROLOGIE2013/hlavni-geneticke-skupiny.htm
Podle zp�sobu a podm�nek vzniku m��eme rozd�lit horniny na magmatick� (vyv�el�), sediment�rn� (usazen�) a metamorfovan� (p�em�n�
https://mi21.vsb.cz/sites/mi21.vsb.cz/files/unit/linearni_algebra_test6.pdf
L in e á rń ı a lg e b ra — 6 . p ře d n á šk a : L in e á rń ı zo b ra ze ń ı D a li b o r
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sobem vyu��v� r�znou sm��itelnost povrchu r�zn�ch materi�l�. Kvantifikovat sm��itelnost lze nap�. kontaktn�m �hlem. Pro jeho exaktn� hodnotu je t�eba prov�st na
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stred Multimedi�ln� v�ukov� text Ekologick� aspekty technick� hydrobiologie Multimedi�ln� texty tvo�� v�znamnou sou��st modern� v�uky. Umo��uj� a usnad�uj� uplat�ov�n� nov�ch vzd�
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Proceedings of ASR 2007 List of authors ASR 2007 - Part B Marek BABIUCH The Usage of Laboratory for Mobile, Wireless and Virtual Computer at the Education Vyu�it�
https://akce.fs.vsb.cz/2007/asr2007/Proceedings/authors/B-2.html
Proceedings of ASR 2007 List of authors ASR 2007 - Part B Marek BABIUCH The Usage of Laboratory for Mobile, Wireless and Virtual Computer at the Education Vyu�it�
http://geologie.vsb.cz/PETROLOGIE2013/metamorfni-faktory-tlak.htm
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lze ��ci, �e hlavn� d�len� metamorfit� je genetick�, kdy hrub� se horniny d�l� do skupin podle typu metamorf�zy, kterou vznikly (region�ln� vs. lok�ln�) a
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