20Radon as Indication of Hartmanns Lattice Network and the Dynamics of Solar-Terrestrial Relationship

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    National Academy of Sciences of RA Electronic Journal of

    NATURAL SCIENCES

    1(2), 2004

    Ecology

    RADON AS INDICATOR OF HARTMANNS LATTICE NETWORK AND THEDYNAMICS OF SOLAR-TERRESTRIAL RELATIONSHIPS

    2 E.A. Saghatelyan, 1Yu.G. Aghbalyan, 2 L.A. Petrosyan, 1 L.A. Araratyan, 1 M.G. Baburyan

    1Center for Ecological-Noosphere Studies NAS RA, 375025, Yerevan, Abovian Str. 68;2Yerevan State Engineering University, 375009, Yerevan, Teryan Str. 105, Republic of Armenia

    Correspondence e-mail : [email protected]

    Key words : objectification, elementary lattice, solar-terrestrial relationships, Hartmanns network.

    ABSTRACT

    For the first time, through radon constituent of terrestrial radiation objectification has been made of elementary lattice of theHartmanns network contoured out by biolocation method. As a matter of record radon concentration correlation regularity in

    positively (+) and negatively (-) polarized nodes have been established:

    1)(

    )(

    +

    Rn

    Rn

    C

    C

    As found out, radon concentration variations in Hartmanns network nodes determine the dynamics of solar-terrestrial relationships.

    INTRODUCTION

    Hartmanns lattice networks are attributed to the category of global energetically active ones which structuralizationoccurs at the level of force-fields energetic, electromagnetic, radiation, and so on. Universally they are expressed at alandscape level and indoors.

    Widely known as geopathogenic zones, Hartmanns network are considered to be one of the most harmful ecologicalrisk factors. The impact of their electromagnetic radiation upon the health of a man is verified by numerous facts ofmedical-epidemiological character published in different countries [2-10] including Armenia [1,2].Hartmanns network is characterized by highest density on the earths surface. The elementary cell of Hartmannsnetwork sized 2x2,5 is oriented NS-WE. Like elementary cells of minerals crystal lattice, Hartmanns network ischaracterized by polarity of nodes. As calculations show, throughout the area of 1km 2 200 000 elementary cells ofHartmanns network are singled out, thus making about 30*10 12 cells allover continental surface only. Structuralizationof similar networks in the process of the Earths evolution and their density evidence their significance that is far

    beyond ecological aspects. Anyway, in geological circles attitude to them is rather skeptic: firstly, there are no sensorsand the networks may be contoured solely through biolocation; secondly, they contradict to accepted geologicalconceptual principles [15]. For this reason, their functional role in the Earths formation has not been studied, yet. Theauthors of this article - specialists in geology, biolocation, measuring instruments, medicine are of the opinion that:1. At present the method of biolocation is sufficiently justified both by investigations of sensitive abilities of a man

    [11-15] and statistical data. Errors in measurements made by the authors through biolocation method applied by 2operators and statistically processed data are within the limits of instrumental methods errors. Therefore, thismethod can be used along with instrumental methods.

    2. The results obtained through biolocation were verified through their objectification by different methods. Particular-ly, objectification of biolocation mapping of Hartmanns network may be carried out by one of the constituents ofthe earths radiation, which intensity may be assessed with the application of available measuring instruments, andthis does not contradict basic principles of metrology. As known, one of the constituents of the earths radiation(alongside with electromagnetic one) is radon natural gas. Very low concentration of radon may be measuredthrough measuring instruments. Thus, objectification of Hartmanns network by radon is quite possible.

    Below, the results of indication of the nodes of Hartmanns network cells by radon and their use for determining thedynamics of solar-terrestrial associations are given.

    STUDY OBJECT AND METHODS

    The testing site is located in the park zone within the limits of Yerevan. In geological structure of the citys territorysoil-covered upper-miocene, quaternary basalts and rocks of salt- and gypsum-bearing layers occur. According togeology-geophysical data, a number of faults cross the citys territory, to which Hrazdan fault and Yerevan flexure

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    identified in the central part of the city, are attributed. Its boundary lies between bared quaternary lava sediments in thenorth and sedimentary layer in the south ( Fig. 1 ).The testing site is located southwest some2km far from Hrazdan fault and about700m - from Yerevan flexure. Bedrocksof the testing site are basalts. There areno maps of emanation survey of the city.According to data on reconnaissanceemanation survey made for two faults bythe Institute of Geophysics and Seismolo-gy in 1991, the testing site is attributed toterritories characterized by negative ano-maly of radon emanation field.Biolocation mapping of the site was con-ducted by two operators separately. Thesigns of polarized nodes (+) or (-) (here-after referred to as positive or negativenodes) were determined by the turn ofthe iron rod clockwise or counter-clock-wise in correspondence with Amperes

    rule. The results obtained independently by the two operators turned out to beidentical and were verified by data of

    polar nodes photometry determining theirdifferences and complex composition ofradiation with radon constituent.To identify the polar nodes of Hartmanncells, special polyethylene balloons 60 m 3 each were adjusted to each of the nodes.The balloons were arranged in soil cover hollows at a depth of 20 cm and thoroughly isolated. The bottom of the

    balloons was kept open so as to collect emitted radon. Inside the balloon, a vertical metal tube with a large amount ofholes was placed, this assuring minimal hydraulic resistance during the operation of the sucking pump of radon meter.Through a flexible hose the metal tube was attached to the entry block of radon meter in which an -radiation adsorbing

    filter was placed. The radon meter pump hoses were attached to the balloons. The measurements of -radiation of radonaerosols and its daughter isotopes adsorbed on the filter while blowing air through it were made applying a portableaerosol-gas radon meter of RV-4 type. The radon meter is designated for measuring concentrations of - and -radioactive gases. The advantage of the instrument is a wide range of measurements from 0,27 to 270 Bk/l.Errors of measurements are from 5 to 31,5%, speed of calculation - 400 and 10 imp/min respectively.The measurements were made for each of the balloons in a 30 min. interval registering the number of impulsescorresponding to decay period of R n-222 radionuclides. Re-calculation of radon concentration impulses was madethrough 2 Thomas and Markov formulas. As only 1 radon meter is available, the impulses in positive and negativenodes of Hartmanns network cells were measured alternately. The measurements were made when the weather wasdry: during magnetic storms and solar eruptions and in geo-magnetically stable conditions mainly from 10 00 till 24 00.

    RESULTS AND DISCUSSIONS

    The analysis of 80 measurements of radon concentration in positive and negatives nodes in Hartmanns network cellsallowed to identify the following regularity: irrespective of geomagnetic situation relation of radon concentration in

    positive node to that in negative one is always above 1 ( Fig. 2 )

    1)(

    )(

    +

    Rn

    Rn

    C

    C .

    This ratio increases depending on geo-magnetic situation: it is minimal when geo-magnetic field is stable: the increasein radon concentration coincides with solstice and falls at an interval between 12 00-13 00, and reaches its maximumduring solar eruptions, when the increase in radon concentration in positive node loses its dependence from the time ofsolstice. Depending on geo-magnetic situation this ratio varies within rather a wide range: 1,2-12,5 ( Fig. 2 ).The comparative analysis of soil radon behavior in polar nodes of a Hartmanns network cell allowed revealing thefollowing peculiarities conditioned by the dynamics of solar-terrestrial relationships.September and the first decade of October were characterized by a relatively stable geo-magnetic field. Radon maximal

    value in positive node coincides with solstice and then begins to decline. Radon concentration in negative node is cha-

    Fig. 2. Schematic map of fault of Yerevan

    Fault

    Hrazdan River

    Pilot Polygon

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    Fig. 2 . Relations of Radon Concentrations in positive and negative nodes of Hartmann`s network

    0

    1

    2

    3

    4

    5

    6

    7

    8

    9

    10

    11

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    13

    13.IX 21.IX 23.IX 24.IX 3.X 7.X 9.X 10.X 23.X 25.X 29.X 1.XI 5.XI 8.XI

    Date

    Rn C(+)Rn C(-)

    020406080

    100120140160

    1 0 : 5

    0

    1 1 : 3

    5

    1 2 : 2

    0

    1 3 : 0

    5

    1 3 : 5

    0

    1 4 : 3

    5

    1 5 : 2

    0

    1 6 : 0

    5

    1 6 : 5

    0

    1 8 : 5

    5

    1 9 : 4

    0

    2 0 : 2

    5

    2 1 : 1

    0

    2 1 : 5

    5

    2 2 : 4

    0

    2 3 : 2

    5

    t

    Bk/l

    C Rn at negative nodeC Rn at positive node

    Fig. 3 . Measurements on 29.10.2003.

    0

    20

    4060

    80

    100

    120

    140

    160

    11:20 13:50 14:30 18:40 20:10 21:40 23:30t

    Bk/l

    C Rn at positive nodeC Rn at negative node

    Fig. 4 . Measurements on 01.11.2003

    racterized by sinusoidalvibrations in the interval(105) Bk/l. Radon con-centration relation in the

    polar nodes

    +

    Rn

    Rn

    C C

    vari-

    es from 1,2 to 3 ( Fig. 2 ).The strongest geo-mag-netic storms for a 11-year solar cycle occurredfrom 29 to 31 October2003. Soil radon monito-ring was conducted onOctober 29 the day ofthe first geomagneticstorm and solar flares,from 10 50 till 23 25 ( Figs.2, 3 ). Data analysis allo-wed identifying the cha-

    racter of radon variationsin negative node duringthe whole monitoring

    process: relativelysmooth, with sinusoidalvibrations. Variation in-terval is (10 5) Bk/l .In contrast to negativenode, radon concentrati-on variations in positivenode are characterized

    by significant variability,max constant values

    being of the order of 55-65 Bk/l . From 12 30 till

    1930

    +

    Rn

    Rn

    C C

    ratio varies

    within 1,5-9.A series of strongest eru-

    ptions (force 35 andhigher) on the Sun occu-rred on November 2,2003. As a result a gase-ous cloud weighting bil-lions of tons turned mo-

    ving towards the earth.The third eruption force20 occurred on Novem-

    ber 4.Soil radon monitoringwas conducted the day

    before the first eruption -on November 1, and af-ter the eruptions - on

    November 8.On November 1 monito-ring was conducted inthe interval 11 20 till 24 15.

    In negative node, soil radon variations continued keeping their low values from 11 20 till 18 40. The character of variationsis sinusoidal, radon level (10 5) Bk/l like that in geomagnetic ally stable days. From 18 40 smooth elevation of radonlevel is registered that reaches 35 Bk/l at 23 30.In positive node soil radon is characterized by contrasting ranges max value making 130 Bk/l at 20 55. ( Fig. 4 ).

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    Difference in ratio

    +

    Rn

    Rn

    C C

    varies in the limits 1,4-12,5 ( Fig. 2 ).

    On November 8, 2003 radon monitoring was conducted during time period from 10 35 to 00 30 after solar flare. Data ana-lysis showed a progressive increase in radon levels in the both positive and negative Hartmann nodes. The reduction oftime length of soil radon with sinusoid variations and concentration of (10 5) Bk/l (in the period of 10 35 13 35) and itssmooth increase up to 95 Bk/l close to 00 35 was established in the negative node.

    In the positive node the increase of soil radon up to 150 Bk/l was established. Two slots of radon increase with stableretention were assigned:First slot from 12 00 to 22 15: CRn+ 110 Bk/lSecond slot from 23 45 to 00 30: CRn+ 150 Bk/l ( Fig. 5 ).

    Difference in ratio

    +

    Rn

    Rn

    C C

    varies in

    the limits 1,5 8 ( Fig 2, 5 ).Analysis of the dynamics of radonvariations in the polar nodes ofHartmann lattice network before andafter solar flares established pro-gressive accumulation of radon in

    both nodes. In negative node suchan increase is characterized by re-duction of interval of low (10 5)Bk/l sinusoid variations of radon theday before the first eruption by one/third, some days after the seconderuption by two/third. Multiplelong-term rises in radon level in po-sitive node is clearly expressed bydiagrams ( Fig. 4, 5 ).

    Fig. 5 . Measurements on 08.11.2003

    In fact, the increasing dynamics of soil radon concentrations in the polar nodes of Hartmanns network cells reflects the

    dynamics of intensification of tense state of the earths crust.All the experimental data testify to the fact that such a state directly depends on the intensity of solar eruptions, forerun

    geomagnetic situation, and is a consequence not only of terrestrial endogen processes, as accepted.The provided data evidence different functional significance of polar nodes of a Hartmanns network cell.

    Radon concentration variations in polar nodes of Hartmanns network cells and ratio

    +

    Rn

    Rn

    C C

    determine the dynamics of

    cause-and-effect solar-terrestrial relationships in different geo-magnetic conditions and solar eruptions.The data obtained testify to different functional roles of polar nodes of a Hartmanns network cell in solar-terrestrialrelationships and allow treating them as a resonant matrix of the Earth determining the dynamics of cause-and-effectsolar-terrestrial relationships.

    CONCLUSION

    1. Indication of nodes of an elementary cell of Hartmanns network by soil radon allows to reveal a clearly expressed

    relation of polar nodes radon in the cell 1)(

    )(

    +

    Rn

    Rn

    C

    C .

    2. The presence of about 120*10 12 polar nodes of Hartmanns network on continental surface allows to treat them as aresonant structures of the Earth.

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    Bk/l

    C Rn at negative nodeC Rn at positive node

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